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Record #170943:

Depositional and diagenetic environments of the Triassic and Lower Jurassic succession of Svalbard / Atle Mørk, Ragnar Knarud, David Worsley.

Title: Depositional and diagenetic environments of the Triassic and Lower Jurassic succession of Svalbard / Atle Mørk, Ragnar Knarud, David Worsley.
Author(s): Mørk, Atle.
Knarud, Ragnar.
Worsley, David.
Date: 1982.
Publisher: Calgary, AB: Canadian Society of Petroleum Geologists
In: Arctic geology and geophysics : proceedings of the Third International Symposium on Arctic Geology. (1982.),
Abstract: Both potential source and reservoir rocks are found in this succession. Authors present revised lithostratigraphical scheme, then review histories of major units. Succession is dominated by clastic sediments deposited in marine environments on relatively stable platform between 45 and 60 deg.N in temperate climate. Thickness variations can be directly related to differential downwarping over series of faults. Facies have similar, more complex patterns. Progradations occur from both east and west. Rhaetoliassic is most complete in east. Results of diagenetic and organic geochemical studies are discussed in sedimentation context.
Notes:

In: Arctic geology and geophysics : proceedings of the Third International Symposium on Arctic Geology / Ashton F. Embry, Hugh R. Balkwill, eds.

Keywords: 550.4 -- Geochemistry.
551.3.051 -- Sedimentation and stratification.
551.76 -- Mesozoic.
553.9 -- Hydrocarbon minerals.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*32) -- Svalbard.
SPRI record no.: 170943

MARCXML

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100 1# ‡aMørk, Atle.
245 10 ‡aDepositional and diagenetic environments of the Triassic and Lower Jurassic succession of Svalbard /‡cAtle Mørk, Ragnar Knarud, David Worsley.
260 ## ‡aCalgary, AB :‡bCanadian Society of Petroleum Geologists,‡c1982.
300 ## ‡ap. 371-398 :‡bill., diags., tables, maps.
500 ## ‡aIn: Arctic geology and geophysics : proceedings of the Third International Symposium on Arctic Geology / Ashton F. Embry, Hugh R. Balkwill, eds.
520 3# ‡aBoth potential source and reservoir rocks are found in this succession. Authors present revised lithostratigraphical scheme, then review histories of major units. Succession is dominated by clastic sediments deposited in marine environments on relatively stable platform between 45 and 60 deg.N in temperate climate. Thickness variations can be directly related to differential downwarping over series of faults. Facies have similar, more complex patterns. Progradations occur from both east and west. Rhaetoliassic is most complete in east. Results of diagenetic and organic geochemical studies are discussed in sedimentation context.
650 07 ‡a550.4 -- Geochemistry.‡2udc
650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc
650 07 ‡a551.76 -- Mesozoic.‡2udc
650 07 ‡a553.9 -- Hydrocarbon minerals.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*32) -- Svalbard.‡2udc
700 1# ‡aKnarud, Ragnar.
700 1# ‡aWorsley, David.
773 0# ‡7nnam ‡aAshton F. Embry, Hugh R. Balkwill, eds. ‡tArctic geology and geophysics : proceedings of the Third International Symposium on Arctic Geology. ‡dCalgary, AB : Canadian Society of Petroleum Geologists, 1982. ‡wSPRI-170709
916 ## ‡aJP
917 ## ‡aUnenhanced record from Muscat, imported 2019
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