Öl und Gas Samllcap Perlen! - 500 Beiträge pro Seite
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Meistdiskutierte Wertpapiere
Platz | vorher | Wertpapier | Kurs | Perf. % | Anzahl | ||
---|---|---|---|---|---|---|---|
1. | 1. | 17.936,50 | +0,21 | 210 | |||
2. | 2. | 180,01 | +0,01 | 106 | |||
3. | 3. | 8,6400 | +4,22 | 85 | |||
4. | 4. | 0,0164 | +0,61 | 75 | |||
5. | 7. | 1,0000 | +3,63 | 42 | |||
6. | 6. | 2.303,32 | -0,02 | 42 | |||
7. | 8. | 6,7280 | +0,81 | 38 | |||
8. | 5. | 3,8775 | +5,01 | 34 |
Eine der besten Chancen zur Zeit ist für mich:
Dover Peroleum!
DVPC
WKN:551365
handelbar nur in New York
aufgrund der letzten Presseaussendungen werde ich mir heute Montag ein paar DVPC reinlegen!
http://www.newsalert.com/bin/digest?Symbol=dvpc#news
Ölfelder im Golf von Suez lassen auf mehr hoffen!
Achtung! diese Aktie ist ein Pink Sheet!
Wer hat noch Öl Smallcaps auf Lager?
morchel
Dover Peroleum!
DVPC
WKN:551365
handelbar nur in New York
aufgrund der letzten Presseaussendungen werde ich mir heute Montag ein paar DVPC reinlegen!
http://www.newsalert.com/bin/digest?Symbol=dvpc#news
Ölfelder im Golf von Suez lassen auf mehr hoffen!
Achtung! diese Aktie ist ein Pink Sheet!
Wer hat noch Öl Smallcaps auf Lager?
morchel
Ein paar finden Sie in meinem mini Thread.
Wenn Sie auf Pink Sheet stehen, kann ich Ihnen noch ein paar nennen.
Wenn Sie auf Pink Sheet stehen, kann ich Ihnen noch ein paar nennen.
Ich denke Hadro wird noch profitieren.
Auch in Deutschland handelbar 626679.
Gruß
MP
Auch in Deutschland handelbar 626679.
Gruß
MP
DOVER PETROLEUM CORP - Other OTC: DVPC
Exchange QuoteLast Change (%) Bid (size) Ask (size) Trade Time
0.70 0.41 (36.94) 0 (0) 0 (0) 09:39
Day Volume Last Size Open High Low
250,500 5,000 0.83 0.84 0.68
morchel was sagst du dazu sollte mn doch wohl eher warten
Exchange QuoteLast Change (%) Bid (size) Ask (size) Trade Time
0.70 0.41 (36.94) 0 (0) 0 (0) 09:39
Day Volume Last Size Open High Low
250,500 5,000 0.83 0.84 0.68
morchel was sagst du dazu sollte mn doch wohl eher warten
URMP.OB
Die sind gerade am rumbohren in Canada!
Ergebnisse werden erwartet!
Wenn sie was gutes erboren dann explodiert das Teil
Gruß
http://biz.yahoo.com/bw/030102/22151_1.html
Die sind gerade am rumbohren in Canada!
Ergebnisse werden erwartet!
Wenn sie was gutes erboren dann explodiert das Teil
Gruß
http://biz.yahoo.com/bw/030102/22151_1.html
Thread eröffnet und -50% wolltet ihr eure papiere noch losbekommen
Morchchel sowas macht man doch nicht aber das ist normal bis jetzt sind 80% aller vorstellungen von morchel min. um 20% gefallen am selben tag
Morchchel sowas macht man doch nicht aber das ist normal bis jetzt sind 80% aller vorstellungen von morchel min. um 20% gefallen am selben tag
Morchel,absolut!! heute nachkaufen
bei der URMP wär ich vorsichtig; hab mal nachgeguckt, die gehören zu ner promotionagentur, uups wollt sagen VC, aus der howe street, ebenfalls VC
die haben ein ziemlich bescheidenes portfolio, alles so im cent bereich, wenn ich mich recht erinnere.
zu DVPC
jetzt wissen wir wenigstens warum die in der letzten PR ihren butt in extrafettgedruckt gecovert haben...
das war einfach zu auffällig.
die haben ein ziemlich bescheidenes portfolio, alles so im cent bereich, wenn ich mich recht erinnere.
zu DVPC
jetzt wissen wir wenigstens warum die in der letzten PR ihren butt in extrafettgedruckt gecovert haben...
das war einfach zu auffällig.
Hallo loss_pro
Was auch immer eine VC ist .mich reizt das Potential bei Positivem Drill!
http://www.apioil.net/s/AthabascaProject.asp?ReportID=29292
hoffe es geht gut
Gruß
Was auch immer eine VC ist .mich reizt das Potential bei Positivem Drill!
http://www.apioil.net/s/AthabascaProject.asp?ReportID=29292
hoffe es geht gut
Gruß
VC sollte in diesem fall für venture capital gesellschaft stehen und zweitens vancouver. alle klarheiten entgültig beseitigt?
@ uh1d
na heute hast noch kein glück; kam gerade über´n ticker:
Uranium Power Corporation: Deep Drilling Program Test Phase to Begin On the 7-32 Well Athabasca Oil Prospect, Fort McMurray Alberta
Business Wire - January 06, 2003 13:13
CALGARY, Alberta--(BUSINESS WIRE)--Jan. 6, 2003--Uranium Power Corporation (OTCBB:URMP)(DAX:URP) The Company is pleased to report that as of 8:00 a.m. Mountain Standard Time today the 7-32 well has reached a depth of 2347 meters (7700 feet).
Initially, a four-inch core sample, which may be 18 meters long, is being cut prior to logging the well from 1651 meters (5417 feet) to the bottom of the hole. Included in the logging will be sonic, neutron density, and velocity logs to identify fracture zones with porosity and/or oil and gas. Based on log results, several prospective zones which have previously recorded oil and/or gas shows will be tested. The coring/logging/testing program is expected to take 3 or 4 days to complete. Warren Hunt, consulting Geologist comments, "The testing program may be very positive as similar producing fields from fractured reservoirs were only discovered after logging and testing."
The Company shall continue to release further information on receipt of the same.
Safe Harbor statement under the Private Securities Litigation Reform Act of 1995: Except for historical information contained herein, the matters discussed in this press release are forward-looking statements that involve risks and uncertainties, including but not limited to economic, competitive, governmental and technological factors effecting the Company`s operations, markets, products and prices and other factors discussed in the Company`s various filings with the Securities and Exchange Commission.
CONTACT: Uranium Power Corporation
Steve McGuire, 800/877-1626
Randal Pow, 888/858-7759
investor@apioil.net
www.apioil.net
na heute hast noch kein glück; kam gerade über´n ticker:
Uranium Power Corporation: Deep Drilling Program Test Phase to Begin On the 7-32 Well Athabasca Oil Prospect, Fort McMurray Alberta
Business Wire - January 06, 2003 13:13
CALGARY, Alberta--(BUSINESS WIRE)--Jan. 6, 2003--Uranium Power Corporation (OTCBB:URMP)(DAX:URP) The Company is pleased to report that as of 8:00 a.m. Mountain Standard Time today the 7-32 well has reached a depth of 2347 meters (7700 feet).
Initially, a four-inch core sample, which may be 18 meters long, is being cut prior to logging the well from 1651 meters (5417 feet) to the bottom of the hole. Included in the logging will be sonic, neutron density, and velocity logs to identify fracture zones with porosity and/or oil and gas. Based on log results, several prospective zones which have previously recorded oil and/or gas shows will be tested. The coring/logging/testing program is expected to take 3 or 4 days to complete. Warren Hunt, consulting Geologist comments, "The testing program may be very positive as similar producing fields from fractured reservoirs were only discovered after logging and testing."
The Company shall continue to release further information on receipt of the same.
Safe Harbor statement under the Private Securities Litigation Reform Act of 1995: Except for historical information contained herein, the matters discussed in this press release are forward-looking statements that involve risks and uncertainties, including but not limited to economic, competitive, governmental and technological factors effecting the Company`s operations, markets, products and prices and other factors discussed in the Company`s various filings with the Securities and Exchange Commission.
CONTACT: Uranium Power Corporation
Steve McGuire, 800/877-1626
Randal Pow, 888/858-7759
investor@apioil.net
www.apioil.net
@Loss-Pro Unklarheiten beseitigt!
Irgendwas scheinen sie ja entdeckt zu haben,ich denke alles wird gut!
Gruß
Irgendwas scheinen sie ja entdeckt zu haben,ich denke alles wird gut!
Gruß
Wenn kein oil,ich hoffe sie hit a Monster!
Das kann man auch vermarkten!
Das kann man auch vermarkten!
wußte gar nicht, daß die in schottischen binnensee bohren...
Da gibts nen Tunnel direkt nach Canada!!!
Aber von mir hast das nicht!!!
Aber von mir hast das nicht!!!
cool, da gibt´s nicht zufällig ne btreibergesellschaft á la eurotunnel, die gerade in eine OTC-shell reverse merged wird? SHIT.PK oder so?
RICHTIG!!!
Ich sag doch alles wird gut
Ich sag doch alles wird gut
Morchel,was fuer morgen FRCD,ANSCHAUEN!!!!
Morchel,guter kauf @0.50.Du alter Fuchs
Ergebnisse sollen kommen uber den Drill!
Ich hoffe es steckt mehr als nur Spekulation in dem heutigem Kursanstieg! Morgen oder übermorgen sollen Ergebnisse folgen. Es geht um urmp.ob
In dieser Gegend wurde aber schon mal Öl gefunden sieh
http://biz.yahoo.com/rc/030106/energy_shellcanada_blast_2.ht…
Gruß
Ich hoffe es steckt mehr als nur Spekulation in dem heutigem Kursanstieg! Morgen oder übermorgen sollen Ergebnisse folgen. Es geht um urmp.ob
In dieser Gegend wurde aber schon mal Öl gefunden sieh
http://biz.yahoo.com/rc/030106/energy_shellcanada_blast_2.ht…
Gruß
Ich hoffe es geht nicht nur um Spekulationen bei dem heutigen Kursanstieg von urmp.ob. Ergebnisse des Drills sollen wohl morgen oder übermorgen folgen!
In dieser Gegend wurde aber schon scheinbar was Brauchbares gefunden!
http://biz.yahoo.com/rc/030106/energy_shellcanada_blast_2.be… stockhouse wird mehr drüber diskutiert oder gestritten!
http://www.stockhouse.com/bullboards/forum.asp?symbol=URMP&t…
In dieser Gegend wurde aber schon scheinbar was Brauchbares gefunden!
http://biz.yahoo.com/rc/030106/energy_shellcanada_blast_2.be… stockhouse wird mehr drüber diskutiert oder gestritten!
http://www.stockhouse.com/bullboards/forum.asp?symbol=URMP&t…
kam gerade rein:
Uranium Power Corporation: Progress Report Athabasca Oil Prospect Fort Mcmurray Alberta Three Potential Pay Zones Identified
Business Wire - January 09, 2003 14:16
CALGARY, Alberta, Canada--(BUSINESS WIRE)--Jan. 9, 2003--
Core Sampling And Logging Completed
Uranium Power Corporation (OTCBB:URMP)(DAX:URP) The Company is pleased to report that Schlumberger has completed a suite of logs on the AOC 7-32 well from 1,600 to 2,336 meters (an interval of 2414 feet) which includes compensated neutron, liphodensity, natural gamma ray spectrometry, micro imaging and high resolution lateral logs. Schlumberger will have completed the processing of the log data, which will include a FMI log by late today.
Nabors Drilling have completed the coring program and have cut 12.9 meters (42.3 feet) of core which is being sent for analysis. Bill Ghazar, the well site geologist, reports high gravity oil shows as well as up to 50 percent sand content in the core. Ross Crane, P.Eng of Spectrum 2000, consultant to the company will analyze all the data to date including data from Schlumberger. Mr. Crane has revealed that upon his preliminary review there appears to be at least two intervals evidencing porosity.
Warren Hunt, consulting geologist comments, "Drilling has revealed high gravity oil showings over the 700 meter (2300 foot) drilled interval, numerous fracture systems and abundant angular quartz sand. Drill stem testing of the intervals of interest will commence tomorrow."
The Company shall continue to release further information on receipt of the same.
Safe Harbor statement under the Private Securities Litigation Reform Act of 1995: Except for historical information contained herein, the matters discussed in this press release are forward-looking statements that involve risks and uncertainties, including but not limited to economic, competitive, governmental and technological factors effecting the Company`s operations, markets, products and prices and other factors discussed in the Company`s various filings with the Securities and Exchange Commission.
CONTACT: Uranium Power Corporation
Steve McGuire, 800/877-1626
investor@apioil.net
www.apioil.net
or
Uranium Power Corporation
Randal Pow, 888/858-7759
investor@apioil.net
www.apioil.net
Uranium Power Corporation: Progress Report Athabasca Oil Prospect Fort Mcmurray Alberta Three Potential Pay Zones Identified
Business Wire - January 09, 2003 14:16
CALGARY, Alberta, Canada--(BUSINESS WIRE)--Jan. 9, 2003--
Core Sampling And Logging Completed
Uranium Power Corporation (OTCBB:URMP)(DAX:URP) The Company is pleased to report that Schlumberger has completed a suite of logs on the AOC 7-32 well from 1,600 to 2,336 meters (an interval of 2414 feet) which includes compensated neutron, liphodensity, natural gamma ray spectrometry, micro imaging and high resolution lateral logs. Schlumberger will have completed the processing of the log data, which will include a FMI log by late today.
Nabors Drilling have completed the coring program and have cut 12.9 meters (42.3 feet) of core which is being sent for analysis. Bill Ghazar, the well site geologist, reports high gravity oil shows as well as up to 50 percent sand content in the core. Ross Crane, P.Eng of Spectrum 2000, consultant to the company will analyze all the data to date including data from Schlumberger. Mr. Crane has revealed that upon his preliminary review there appears to be at least two intervals evidencing porosity.
Warren Hunt, consulting geologist comments, "Drilling has revealed high gravity oil showings over the 700 meter (2300 foot) drilled interval, numerous fracture systems and abundant angular quartz sand. Drill stem testing of the intervals of interest will commence tomorrow."
The Company shall continue to release further information on receipt of the same.
Safe Harbor statement under the Private Securities Litigation Reform Act of 1995: Except for historical information contained herein, the matters discussed in this press release are forward-looking statements that involve risks and uncertainties, including but not limited to economic, competitive, governmental and technological factors effecting the Company`s operations, markets, products and prices and other factors discussed in the Company`s various filings with the Securities and Exchange Commission.
CONTACT: Uranium Power Corporation
Steve McGuire, 800/877-1626
investor@apioil.net
www.apioil.net
or
Uranium Power Corporation
Randal Pow, 888/858-7759
investor@apioil.net
www.apioil.net
Haben wir einen Ölfanatiker oder einen der sich ein bißchen auskennt in der Runde? Klingt ja erst mal positiv!? Aber die Kursreaktion verwundert mich!(sell on ..!) Abwarten
Achso betrifft URMP.OB
Achso betrifft URMP.OB
hallo suche volltext translator, abacho Translator hat gerade keine Lust bei mir bekomme lehre Seiten wieder. Danke
oder Text gleich übersetzen!?
A wide selection of the medieval floor tiles from Cleeve Abbey were examined and samples selected for petrological analysis. The aims of this analysis were: 1) to establish the sources of supply used and 2) to test the classification erected by Ms Harcourt on the basis of design, quarry size and appearance.
Thirty-one samples were prepared at the Lincoln Ceramic Petrology Laboratory and entered into the Laboratory`s reference collection using the reference codes L2031 to L2062. All were stained using Dickson`s Method in order to distinguish between ferroan calcite, non-ferroan calcite and dolomite.
Sub samples were then submitted to Dr N Walsh for IPCS analysis and the resulting data were recorded in an Excel 5 spreadsheet.
Results
The samples could be divided into five groups on the basis of their petrological characteristics. In one case a group could be reliably identified as being the products of a well-known tile factory whose products were widely distributed around the Bristol Channel (Vince 1984 Chapter 2: St Bartholomew`s-Type Tiles). These tiles, Harcourt`s Groups 4 and 5, are usually associated with Cleeve Abbey, following Ward-Perkins` publication of the heraldic tiles from the site, but can now be seen to be a minor element in the Cleeve assemblage. Furthermore, it is also clear that they are at the extreme western edge of a distribution which stretches as far north-east as Gloucester. The remaining groups are likely to be of more local origin and can be divided into those in which the inclusions are of Cretaceous origin and those where the inclusions are probably of Devonian origin. The latter tiles are most likely to be of local origin whereas those in the former group probably originated further east. These petrological groups are here given Fabric Group letters, so as not to be confused with the design groups, which have numbers.
Fabric Group A/B
Six samples of this group were examined. By eye the group was subdivided into two, Fabrics A and B, but in thin-section this distinction cannot be sustained. The tiles in this fabric include examples of design groups 1, 2 and 3, together with a rogue example of design group 9 (visually identified as Fabric E).
The petrological characteristics of this fabric are:
Abundant rounded clay pellets, up to 4mm across.
Sparse rounded sandstone and siltstone fragments, up to 1.0mm across.
Abundant quartz silt
Moderate flakes of muscovite up to 0.1mm long
Fabric A/B is distinguishable from Fabrics E and F, to which its ICPS analyses are otherwise very similar, in the quantities of K2O and P2O5 present.
Fabric Group C
Six samples of Fabric C were examined. They include examples of design groups 4 and 5.
The petrological characteristics of this fabric are:
Abundant silt-sized angular quartz
Moderate flakes of muscovite
Moderate fragments of ?altered glauconite
A plot of Nickel vs Chromium content using the ICPS results clearly separates Fabric C from all others.
Fabric Group D
Five examples of Fabric D were examined, all of design group 6.
The petrological characteristics of this fabric are:
Abundant rounded quartz sand, with grains up to 1.5mm across (but mainly less than 0.5mm)
Moderate to abundant rounded grains of altered glauconite, up to 0.4mm across. Some of these grains retain a zoned structure, with a darker core.
A plot of Nickel vs Chromium using the IPCS analyses clearly separates Fabric D from all others.
Fabric Group E/G
Ten examples of Fabric E/G were examined. They include tiles of design groups 7, 8, 8A, 9 and 12.
The petrological characteristics of the fabric are:
Abundant ill-sorted quartz sand with grains up to 0.5mm across
Sparse rounded fragments of Lower Greensand Chert (angular quartz sand c.0.2mm across, in a matrix of silica) up to 1.0mm across
Sparse angular opaque to dark brown iron-rich inclusions up to 3.0mm across (section L2407 only)
Sparse rounded flint up to 1.0mm across.
Abundant clay pellets of varying colour. Some have dark brown staining (?manganese?)
Moderate muscovite flakes up to 0.1mm long.
Fabric G was distinguished visually as having a higher quantity of rounded quartz sand and this is bourne out by petrological analysis. However, it is also clear from this analysis that the range of inclusions in the two fabrics is identical.
Fabric G, however, is distinguishable from the remaining fabrics using the ICPS results, which show a high Barium content for four of the five samples.
Fabric Group F
Four examples of Fabric F were examined, all of design group 11.
The petrological characteristics are:
Abundant angular quartz silt/very fine sand (average c.0.1mm across)
Sparse angular sandstone fragments up to 1.5mm across
Sparse ?Lower Greensand Chert up to 1.0mm across
Sparse rounded flint
Sparse to moderate muscovite up to 0.1mm long
Fabric F is distinguishable from Fabrics A and E, to which it is otherwise very similar, through its lower P2O5 content and higher average K2O content.
Discussion
The main petrological division present in this material is into fabrics which contain wholely or mainly rocks and minerals of likely Cretaceous origin and fabrics containing inclusions of probable Devonian origin. Only one fabric, F, includes material from both sources and even here it is clear that the fabric is mainly tempered with Cretaceous material. The characteristics of these Cretaceous fabrics are:
Rounded quartz sand, often including well-rounded grains, some with brown-stained veins (Fabrics D and G)
Lower Greensand Chert (Fabrics E, G and F)
Flint (Fabrics E, G and F)
Glauconite (Fabrics C and D)
Abundant quartz and muscovite silt (Fabric C)
It is known that this material of ultimate Cretaceous origin is found widely in the sands and gravels of Somerset but that as one moves south and west so the material is mixed with rocks and minerals of south-western origin. Glauconite, especially in quantity and with relatively large grains, is unlikely to occur in these secondary contexts to anything like the same extent as chert and flint and its present in fabric D is an indicator of an origin somewhere close to the outcrop of Cretaceous rocks. Whether its presence as much smaller fragments in Fabric C is also significant for the source of the clay is less certain, especially so since the known distribution of tiles of this type does not include areas on or close to the Cretaceous outcrop (for example, Bristol, Gloucester and Tintern, in addition to Cleeve).
Fine-grained sandstones, often with a high proportion of non-quartzose inclusions (ie. classifiable as greywackes), are the other distictive inclusion type in the Cleeve assemblage. Although only present in two fabric groups, A/B and F, and only common in the former, it should be remembered that fabric group A/B is actually the most common at Cleeve and there is no reason to doubt that fabric group A/B is relatively local, although it is not possible without clay and potential temper samples from the area to show whether or not the raw materials could have been collected on site. The large quantity of clay pellets in Fabric A/B suggests a casual attitude towards clay preparation, although it may simply be a characteristic of the sources used.
Fabric F, which includes a mixture of southwestern and Cretaceous inclusions, is similar in petrology and texture to the fabric of the products of the Donyatt potteries and this may likewise be the source of these tiles.
The ICPS analyses confirm that each of the fabric groups recognised here is chemically distinct. Fabrics D and C are clearly distinguished from the remainder using their Nickel and Chromium contents. Fabric G can be distinguished in four out of five cases by its Barium content whilst the remaining three Fabrics - A/B, E and F - are similar in most respects but can be differentiated by their K2O and P2O5 frequencies.
Statistical analysis of ICPS (added 1999)
In 1999 the Cleeve Abbey data were examined using Principal Components Analysis (the Bonn Archaeological Statistics Package for Windows - WinBASP). Fourteen components were computed by the program, the first of which accounted for the majority of the statistical variation in the dataset, the second of which accounted for next and so on. Some of the petrological groups formed clearly separated clusters whilst others overlapped with neighbouring groups. Using a combination of different components it was possible to separate Fabrics C, D, E and G from each other and from the remaining samples.
The plot of PC2 versus PC4, shown here, is the clearest.
The contribution of the different elements to this plot is shown here. It indicates that Fabric D, tempered with a glauconitic sand, is distinguished by a group of elements: Ni, Co, V, Zr, Yb, Y, Dy and Cu. Fabric G, a quartz and chert sand-tempered fabric, is distinguished by CaO, Sr and Ba.
oder Text gleich übersetzen!?
A wide selection of the medieval floor tiles from Cleeve Abbey were examined and samples selected for petrological analysis. The aims of this analysis were: 1) to establish the sources of supply used and 2) to test the classification erected by Ms Harcourt on the basis of design, quarry size and appearance.
Thirty-one samples were prepared at the Lincoln Ceramic Petrology Laboratory and entered into the Laboratory`s reference collection using the reference codes L2031 to L2062. All were stained using Dickson`s Method in order to distinguish between ferroan calcite, non-ferroan calcite and dolomite.
Sub samples were then submitted to Dr N Walsh for IPCS analysis and the resulting data were recorded in an Excel 5 spreadsheet.
Results
The samples could be divided into five groups on the basis of their petrological characteristics. In one case a group could be reliably identified as being the products of a well-known tile factory whose products were widely distributed around the Bristol Channel (Vince 1984 Chapter 2: St Bartholomew`s-Type Tiles). These tiles, Harcourt`s Groups 4 and 5, are usually associated with Cleeve Abbey, following Ward-Perkins` publication of the heraldic tiles from the site, but can now be seen to be a minor element in the Cleeve assemblage. Furthermore, it is also clear that they are at the extreme western edge of a distribution which stretches as far north-east as Gloucester. The remaining groups are likely to be of more local origin and can be divided into those in which the inclusions are of Cretaceous origin and those where the inclusions are probably of Devonian origin. The latter tiles are most likely to be of local origin whereas those in the former group probably originated further east. These petrological groups are here given Fabric Group letters, so as not to be confused with the design groups, which have numbers.
Fabric Group A/B
Six samples of this group were examined. By eye the group was subdivided into two, Fabrics A and B, but in thin-section this distinction cannot be sustained. The tiles in this fabric include examples of design groups 1, 2 and 3, together with a rogue example of design group 9 (visually identified as Fabric E).
The petrological characteristics of this fabric are:
Abundant rounded clay pellets, up to 4mm across.
Sparse rounded sandstone and siltstone fragments, up to 1.0mm across.
Abundant quartz silt
Moderate flakes of muscovite up to 0.1mm long
Fabric A/B is distinguishable from Fabrics E and F, to which its ICPS analyses are otherwise very similar, in the quantities of K2O and P2O5 present.
Fabric Group C
Six samples of Fabric C were examined. They include examples of design groups 4 and 5.
The petrological characteristics of this fabric are:
Abundant silt-sized angular quartz
Moderate flakes of muscovite
Moderate fragments of ?altered glauconite
A plot of Nickel vs Chromium content using the ICPS results clearly separates Fabric C from all others.
Fabric Group D
Five examples of Fabric D were examined, all of design group 6.
The petrological characteristics of this fabric are:
Abundant rounded quartz sand, with grains up to 1.5mm across (but mainly less than 0.5mm)
Moderate to abundant rounded grains of altered glauconite, up to 0.4mm across. Some of these grains retain a zoned structure, with a darker core.
A plot of Nickel vs Chromium using the IPCS analyses clearly separates Fabric D from all others.
Fabric Group E/G
Ten examples of Fabric E/G were examined. They include tiles of design groups 7, 8, 8A, 9 and 12.
The petrological characteristics of the fabric are:
Abundant ill-sorted quartz sand with grains up to 0.5mm across
Sparse rounded fragments of Lower Greensand Chert (angular quartz sand c.0.2mm across, in a matrix of silica) up to 1.0mm across
Sparse angular opaque to dark brown iron-rich inclusions up to 3.0mm across (section L2407 only)
Sparse rounded flint up to 1.0mm across.
Abundant clay pellets of varying colour. Some have dark brown staining (?manganese?)
Moderate muscovite flakes up to 0.1mm long.
Fabric G was distinguished visually as having a higher quantity of rounded quartz sand and this is bourne out by petrological analysis. However, it is also clear from this analysis that the range of inclusions in the two fabrics is identical.
Fabric G, however, is distinguishable from the remaining fabrics using the ICPS results, which show a high Barium content for four of the five samples.
Fabric Group F
Four examples of Fabric F were examined, all of design group 11.
The petrological characteristics are:
Abundant angular quartz silt/very fine sand (average c.0.1mm across)
Sparse angular sandstone fragments up to 1.5mm across
Sparse ?Lower Greensand Chert up to 1.0mm across
Sparse rounded flint
Sparse to moderate muscovite up to 0.1mm long
Fabric F is distinguishable from Fabrics A and E, to which it is otherwise very similar, through its lower P2O5 content and higher average K2O content.
Discussion
The main petrological division present in this material is into fabrics which contain wholely or mainly rocks and minerals of likely Cretaceous origin and fabrics containing inclusions of probable Devonian origin. Only one fabric, F, includes material from both sources and even here it is clear that the fabric is mainly tempered with Cretaceous material. The characteristics of these Cretaceous fabrics are:
Rounded quartz sand, often including well-rounded grains, some with brown-stained veins (Fabrics D and G)
Lower Greensand Chert (Fabrics E, G and F)
Flint (Fabrics E, G and F)
Glauconite (Fabrics C and D)
Abundant quartz and muscovite silt (Fabric C)
It is known that this material of ultimate Cretaceous origin is found widely in the sands and gravels of Somerset but that as one moves south and west so the material is mixed with rocks and minerals of south-western origin. Glauconite, especially in quantity and with relatively large grains, is unlikely to occur in these secondary contexts to anything like the same extent as chert and flint and its present in fabric D is an indicator of an origin somewhere close to the outcrop of Cretaceous rocks. Whether its presence as much smaller fragments in Fabric C is also significant for the source of the clay is less certain, especially so since the known distribution of tiles of this type does not include areas on or close to the Cretaceous outcrop (for example, Bristol, Gloucester and Tintern, in addition to Cleeve).
Fine-grained sandstones, often with a high proportion of non-quartzose inclusions (ie. classifiable as greywackes), are the other distictive inclusion type in the Cleeve assemblage. Although only present in two fabric groups, A/B and F, and only common in the former, it should be remembered that fabric group A/B is actually the most common at Cleeve and there is no reason to doubt that fabric group A/B is relatively local, although it is not possible without clay and potential temper samples from the area to show whether or not the raw materials could have been collected on site. The large quantity of clay pellets in Fabric A/B suggests a casual attitude towards clay preparation, although it may simply be a characteristic of the sources used.
Fabric F, which includes a mixture of southwestern and Cretaceous inclusions, is similar in petrology and texture to the fabric of the products of the Donyatt potteries and this may likewise be the source of these tiles.
The ICPS analyses confirm that each of the fabric groups recognised here is chemically distinct. Fabrics D and C are clearly distinguished from the remainder using their Nickel and Chromium contents. Fabric G can be distinguished in four out of five cases by its Barium content whilst the remaining three Fabrics - A/B, E and F - are similar in most respects but can be differentiated by their K2O and P2O5 frequencies.
Statistical analysis of ICPS (added 1999)
In 1999 the Cleeve Abbey data were examined using Principal Components Analysis (the Bonn Archaeological Statistics Package for Windows - WinBASP). Fourteen components were computed by the program, the first of which accounted for the majority of the statistical variation in the dataset, the second of which accounted for next and so on. Some of the petrological groups formed clearly separated clusters whilst others overlapped with neighbouring groups. Using a combination of different components it was possible to separate Fabrics C, D, E and G from each other and from the remaining samples.
The plot of PC2 versus PC4, shown here, is the clearest.
The contribution of the different elements to this plot is shown here. It indicates that Fabric D, tempered with a glauconitic sand, is distinguished by a group of elements: Ni, Co, V, Zr, Yb, Y, Dy and Cu. Fabric G, a quartz and chert sand-tempered fabric, is distinguished by CaO, Sr and Ba.
das ist ein echter morchel
knapp -50% in wenigen Tagen - das schafft nur morchel
knapp -50% in wenigen Tagen - das schafft nur morchel
#26
Wann hat er denn gekauft am Montag? Javio neiddu
Wann hat er denn gekauft am Montag? Javio neiddu
Empfehlung in #1 am 05.01
also wird er am Montag gekauft haben wie er schrieb
also wird er am Montag gekauft haben wie er schrieb
Das Tief war Montag bei fast 0,4 jetzt haben wir 0,64
also eher plus 50%,kann aber auch umgekehrt gewesen sein!
Gruß
also eher plus 50%,kann aber auch umgekehrt gewesen sein!
Gruß
Zu welchem Zeitpunkt Herr Morchel nun gekauft hat ist mir sehr egal, wollte eigentlich nur einen komplett Translator!
Warum ist der Kurs sehr starkt gefallen.
Morchel anzugreifen ist sehr unfair. Ihr werdet über die Firma nacht die Finger legen.
recife
Morchel anzugreifen ist sehr unfair. Ihr werdet über die Firma nacht die Finger legen.
recife
Hallo.
Dover hatte leider Pesch beim ersten Bohrloch, aus technischen Gründen. Der Bohrmeister hat leider nicht gute Arbeit geleistet - wurde auch sofort entlassen. Dover mußte aus vertraglichen Gründen ab einem neuen Standort bohren. Hiernach darf sie wieder an am ersten Loch weiterbohren. Die Schätzungen liegen weiter sehr hoch.
1 Bohrung ca. 50.000.000 Barral Oel. Wenn das 2 te Bohrloch erschlossen ist, dürfen sie nach Vertrag wieder zum ersten ZÜRÜCK,
Dover hat für 15 Oelfelder Konz. . davon sind 6 voll finanziert.
Viel Spass noch, ich bin keiner, der den Kurs puschen will, macht was IHR wollt.
RECIFE
Dover hatte leider Pesch beim ersten Bohrloch, aus technischen Gründen. Der Bohrmeister hat leider nicht gute Arbeit geleistet - wurde auch sofort entlassen. Dover mußte aus vertraglichen Gründen ab einem neuen Standort bohren. Hiernach darf sie wieder an am ersten Loch weiterbohren. Die Schätzungen liegen weiter sehr hoch.
1 Bohrung ca. 50.000.000 Barral Oel. Wenn das 2 te Bohrloch erschlossen ist, dürfen sie nach Vertrag wieder zum ersten ZÜRÜCK,
Dover hat für 15 Oelfelder Konz. . davon sind 6 voll finanziert.
Viel Spass noch, ich bin keiner, der den Kurs puschen will, macht was IHR wollt.
RECIFE
Dover ist die Perle der nahen Zukunft.
recife
Fragen gerne.
recife
recife
Fragen gerne.
recife
Er ist Super eingestiegen.
Das schafft keiner im letzten Jahr. Prima
recife
Das schafft keiner im letzten Jahr. Prima
recife
Lacht nur - morchel wird recht behalten. Viel Spass noch mit mit euren unfairen Behauptungen.
recife
recife
Lachen ist gut, aber...........
Manchmal falsch, wenn man die Firma nicht kennt.
Viel Spass noch
recife
Manchmal falsch, wenn man die Firma nicht kennt.
Viel Spass noch
recife
Kennt du die Hinterkünde??????
Warum immer angreifen und auslachen. Wenn Du es besser weisst rede einfach, aber bitte nicht so.
recife
Warum immer angreifen und auslachen. Wenn Du es besser weisst rede einfach, aber bitte nicht so.
recife
Diese Anfeindung finde ich nicht fair, IHR werdet Euch noch wundern, es hat sich alles nur um 2-3 Wochen verschoben. Es Infos, bitte informiert EUCH zuerst, bevor Ihr lacht
refife
refife
Egal, spielt keine Rolle.
recife
recife
Hallo Javier,
bitte ganz leise, wer lacht zum Schluss ---ich hoffe Du auch.
recife
bitte ganz leise, wer lacht zum Schluss ---ich hoffe Du auch.
recife
Sorry für die falsche Reihenfolge,
recife
recife
@recife
Ich hoffe der Rest Deiner Nacht hat geklappt!
Deine Postings verwirren mich sehr!
Wird schon!
Ich hoffe der Rest Deiner Nacht hat geklappt!
Deine Postings verwirren mich sehr!
Wird schon!
Uranium Power Corporation: Logging and Testing Confirm Massive Reservoir Potential
Monday January 13, 1:48 pm ET
Athabasca Oil Prospect, Fort McMurray Alberta
CALGARY, Alberta--(BUSINESS WIRE)--Jan. 13, 2003-- Uranium Power Corporation (OTC BB:URMP)(DAX:URP) The Company is pleased to report limited testing at the 7-32 well has now been conducted with positive results. During operations rock particles were recovered, oil and gas shows were confirmed, cores were cut and analyzed, logs were run and 3 intervals tested confirming the potential of massive fracture reservoirs containing unlimited reserves under the Company`s extensive land holdings comprising 97 square miles.
The logs revealed a number of fracture systems only 2 of which are verified by testing. A third interval at the bottom of the hole also was tested, which was cored but not logged and observed to be fractured with oil and gas shows. The 3 tested intervals are 1645 - 1670 meters (82 feet), 1755 - 1800 meters (148 ft) and 2345 -2363 meters (59 feet).
All three intervals yielded fluid recoveries with gas shows and good formation pressures which confirm permeability. An analysis of these samples indicate they are largely comprised of filtrate that invaded the fracture systems during drilling operations. The filtrate recoveries and gas shows confirm the presence of oil and gas in fracture basement rocks.
The Company`s consultants recommend a testing period of several days is required to allow the fractures to be cleared of the invading filtrate to enable oil and gas to enter the well bore. This testing procedure cannot be accomplished with the drill rig now being utilized. This rig will be released today and a service rig will be immediately contracted to continue this testing procedure. The program will include running a string of tubing to swab all of the drill mud out of the well. The total length of the well (2363 meters or 7750 feet) would then release oil and gas from all permeable fracture zones which may result in oil and gas production. The fracture zones above 1650 meters may have been damaged by drilling mud remaining in the well over 8 years but may have similar permeability with potential reservoirs as evidenced below.
The Company has set up a conference call for 10:00 am Pacific, 1:00 pm Eastern time Tuesday January 14, 2003 for further information. Lorne Inglis, Director and Petroleum Geologist; Doug Cannaday, President and Vern Stone, Drilling Engineer will be in attendance. Please call 10 -15 minutes prior to Presentation.
Participant Dial-in Numbers:
TOLL-FREE 1-800-814-3911
TOLL/INTERNATIONAL 1-416-640-4127
Safe Harbor statement under the Private Securities Litigation Reform Act of 1995: Except for historical information contained herein, the matters discussed in this press release are forward-looking statements that involve risks and uncertainties, including but not limited to economic, competitive, governmental and technological factors effecting the Company`s operations, markets, products and prices and other factors discussed in the Company`s various filings with the Securities and Exchange Commission.
--------------------------------------------------------------------------------
Contact:
Uranium Power Corporation
Steve McGuire, 800/877-1626
or
Uranium Power Corporation
Randal Pow, 888/858-7759
investor@apioil.net
www.apioil.net
Monday January 13, 1:48 pm ET
Athabasca Oil Prospect, Fort McMurray Alberta
CALGARY, Alberta--(BUSINESS WIRE)--Jan. 13, 2003-- Uranium Power Corporation (OTC BB:URMP)(DAX:URP) The Company is pleased to report limited testing at the 7-32 well has now been conducted with positive results. During operations rock particles were recovered, oil and gas shows were confirmed, cores were cut and analyzed, logs were run and 3 intervals tested confirming the potential of massive fracture reservoirs containing unlimited reserves under the Company`s extensive land holdings comprising 97 square miles.
The logs revealed a number of fracture systems only 2 of which are verified by testing. A third interval at the bottom of the hole also was tested, which was cored but not logged and observed to be fractured with oil and gas shows. The 3 tested intervals are 1645 - 1670 meters (82 feet), 1755 - 1800 meters (148 ft) and 2345 -2363 meters (59 feet).
All three intervals yielded fluid recoveries with gas shows and good formation pressures which confirm permeability. An analysis of these samples indicate they are largely comprised of filtrate that invaded the fracture systems during drilling operations. The filtrate recoveries and gas shows confirm the presence of oil and gas in fracture basement rocks.
The Company`s consultants recommend a testing period of several days is required to allow the fractures to be cleared of the invading filtrate to enable oil and gas to enter the well bore. This testing procedure cannot be accomplished with the drill rig now being utilized. This rig will be released today and a service rig will be immediately contracted to continue this testing procedure. The program will include running a string of tubing to swab all of the drill mud out of the well. The total length of the well (2363 meters or 7750 feet) would then release oil and gas from all permeable fracture zones which may result in oil and gas production. The fracture zones above 1650 meters may have been damaged by drilling mud remaining in the well over 8 years but may have similar permeability with potential reservoirs as evidenced below.
The Company has set up a conference call for 10:00 am Pacific, 1:00 pm Eastern time Tuesday January 14, 2003 for further information. Lorne Inglis, Director and Petroleum Geologist; Doug Cannaday, President and Vern Stone, Drilling Engineer will be in attendance. Please call 10 -15 minutes prior to Presentation.
Participant Dial-in Numbers:
TOLL-FREE 1-800-814-3911
TOLL/INTERNATIONAL 1-416-640-4127
Safe Harbor statement under the Private Securities Litigation Reform Act of 1995: Except for historical information contained herein, the matters discussed in this press release are forward-looking statements that involve risks and uncertainties, including but not limited to economic, competitive, governmental and technological factors effecting the Company`s operations, markets, products and prices and other factors discussed in the Company`s various filings with the Securities and Exchange Commission.
--------------------------------------------------------------------------------
Contact:
Uranium Power Corporation
Steve McGuire, 800/877-1626
or
Uranium Power Corporation
Randal Pow, 888/858-7759
investor@apioil.net
www.apioil.net
Ich weiß zwar nicht ob das eine Perle ist,aber
hört sich aber erstmal gut an!?
http://finance.yahoo.com/q?s=tglef.ob&d=t
schönen Abend noch
hört sich aber erstmal gut an!?
http://finance.yahoo.com/q?s=tglef.ob&d=t
schönen Abend noch
Ist gerade am Detonieren diese Aktie !!
Weiß jemand mehr als keiner??
http://finance.yahoo.com/q?s=aigi.ob&d=t
Gruß
Weiß jemand mehr als keiner??
http://finance.yahoo.com/q?s=aigi.ob&d=t
Gruß
Adair Oil....sehr gefährlich!
morchel
morchel
Hai, weiß jemand was die so machen?
Es geht um ENVIRO-ENERGY!
http://finance.yahoo.com/q?s=engy.ob&d=t
Danke für Antworten!
Es geht um ENVIRO-ENERGY!
http://finance.yahoo.com/q?s=engy.ob&d=t
Danke für Antworten!
Bei URMP.OB sollen heute die Ergebnisse der Bohrung kommen!
Also wer noch was riskieren will!
Gruß
Also wer noch was riskieren will!
Gruß
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