TY - CHAP
T1 - Depositional history and petroleum geology of the Carboniferous to Cretaceous sediments in the northern part of East Greenland
AU - Stemmerik, Lars
AU - Christiansen, Flemming G.
AU - Piasecki, Stefan
AU - Jordt, Birthe
AU - Marcussen, Christian
AU - Nøhr-Hansen, Henrik
PY - 1993/1/1
Y1 - 1993/1/1
N2 - Major depositional phases of subsidence and basin fill occurred in northern East Greenland during the latest Devonian–earliest Carboniferous, Late Carboniferous, Late Permian–earliest Triassic, mid-Jurassic-earliest Cretaceous, and mid-Cretaceous, and a total of 5-6 km of sediment accumulated. These phases were followed by a phase of Tertiary volcanism and a subsequent period of uplift. Potential source rocks include oil-prone, Upper Carboniferous lacustrine shales, oil-prone Upper Permian marine shales, and gas-prone Upper Jurassic marine shales. The shales are generally immature in outcrop with the exception of areas surrounding larger Tertiary intrusions and areas with a high density of Tertiary sills. In these areas sediments are postmature. The potential source rocks are believed to be adequately buried with respect to oil-generation only in the easternmost part of the area, where they apparently passed into the oil-window during Cretaceous time. In this area four play concepts have been suggested, all with Upper Palaeozoic source rocks and respectively Upper Carboniferous, Upper Permian, Middle Jurassic and Upper Jurassic–Lower Cretaceous reservoirs.
AB - Major depositional phases of subsidence and basin fill occurred in northern East Greenland during the latest Devonian–earliest Carboniferous, Late Carboniferous, Late Permian–earliest Triassic, mid-Jurassic-earliest Cretaceous, and mid-Cretaceous, and a total of 5-6 km of sediment accumulated. These phases were followed by a phase of Tertiary volcanism and a subsequent period of uplift. Potential source rocks include oil-prone, Upper Carboniferous lacustrine shales, oil-prone Upper Permian marine shales, and gas-prone Upper Jurassic marine shales. The shales are generally immature in outcrop with the exception of areas surrounding larger Tertiary intrusions and areas with a high density of Tertiary sills. In these areas sediments are postmature. The potential source rocks are believed to be adequately buried with respect to oil-generation only in the easternmost part of the area, where they apparently passed into the oil-window during Cretaceous time. In this area four play concepts have been suggested, all with Upper Palaeozoic source rocks and respectively Upper Carboniferous, Upper Permian, Middle Jurassic and Upper Jurassic–Lower Cretaceous reservoirs.
UR - http://www.scopus.com/inward/record.url?scp=85008788476&partnerID=8YFLogxK
U2 - 10.1016/B978-0-444-88943-0.50009-5
DO - 10.1016/B978-0-444-88943-0.50009-5
M3 - Chapter in book
AN - SCOPUS:85008788476
SN - 0-444-88943-4
T3 - Norwegian Petroleum Society Special Publications
SP - 67
EP - 87
BT - Arctic geology and petroleum potential
A2 - Vorren, T.O.
A2 - Bergsager, E.
A2 - Dahl-Stamnes, Ø.A.
A2 - Holter, E.
A2 - Johansen, B.
A2 - Lie, E.
A2 - Lund, T.B.
PB - Elsevier
CY - Amsterdam
T2 - Norwegian Petroleum Society Conference 1990
Y2 - 15 August 1990 through 17 August 1990
ER -