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| 02351nam 2200373za 4500 |
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001 | 9.835886 |
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003 | CaOODSP |
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005 | 20221107150753 |
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007 | cr ||||||||||| |
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008 | 170427s1985 oncabd|#ot|||f000 0 eng d |
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040 | |aCaOODSP|beng |
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041 | |aeng|beng|bfre |
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043 | |an-cn-sn|an-cn-nt |
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086 | 1 |aM74-3/85-6E-PDF |
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100 | 1 |aJones, F. W. |
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245 | 10|aStudy of exisiting temperature data from Canadian basins, phase IV |h[electronic resource] / |cF.W. Jones and J.A. Majorowicz. |
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246 | 15|aGeothermics of the Williston Basin in Canada in relation to hydrodynamics and hydrocarbon occurrences |
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260 | |aOttawa : |bEnergy, Mines and Resources Canada, Earth Physics Branch, |c1985. |
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300 | |a76 p. : |bill., maps |
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490 | 1 |aEarth Physics Branch open file = Dossier public de la Direction de la Physique du Globe ; |vno. 85-6 |
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500 | |aTitle from cover. |
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500 | |aAt head of title: Geodynamics Service of Canada = Service géodynamique du Canada. |
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500 | |aDigitized edition from print produced 2017 [by Natural Resources Canada] |
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504 | |aIncludes bibliographical references. |
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520 | 3 |a"Over 8400 bottom-hole temperature (BHT) values from the Canadian part of the Williston Basin have been analysed and a temperature anomaly has been discovered in the Weyburn area of southeastern Saskatchewan. Regional heat flow variations are observed, and these are closely related to the hydrodynamics which is governed by the topography and geology. The blanketing effect of low conductivity shaly formations may cause a temperature anomaly in the south where the thickest Phanerozoic cover exists. However, the Weyburn anomaly can be only partly explained in this way. Hydrodynamics has also contributed to the formation of this temperature anomaly. Preliminary examination of data from the Northwest Territories has commenced"--Abstract. |
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546 | |aIncludes abstract in French. |
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692 | 07|2gccst|aTemperature |
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700 | 1 |aMajorowicz, J. A. |
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700 | 1 |aBurn, C. |
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710 | 1 |aCanada. |bEnergy, Mines and Resources Canada. |
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710 | 1 |aCanada. |bEarth Physics Branch. |
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830 | #0|aOpen file (Earth Physics Branch)|vno. 85-6|w(CaOODSP)9.835819 |
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856 | 40|qPDF|s16.53 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M74-3-85-6-eng.pdf |
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