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Titlebook: Non-standard Problems in Basin Modelling; Yurii Galushkin Book 2016 Springer International Publishing Switzerland 2016 GALO Modeling Progr

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樓主: 戰(zhàn)神
21#
發(fā)表于 2025-3-25 06:17:35 | 只看該作者
The Lithosphere Extension and Hydrocarbon Generation in the Eastern Continental Passive Margin of Inin shallow and deep-water offshore are discussed in detail. The consequences of these differences in the generation of different fractions of hydrocarbons by probable source rocks of the basin are considered also.
22#
發(fā)表于 2025-3-25 11:00:28 | 只看該作者
23#
發(fā)表于 2025-3-25 15:02:16 | 只看該作者
24#
發(fā)表于 2025-3-25 17:13:38 | 只看該作者
25#
發(fā)表于 2025-3-25 21:29:13 | 只看該作者
rs a valuable resource for all graduate students and professionals interested in numerical modelling of the thermal evolution of sedimentary basins. It will also be of great interest to petroleum geologists eng978-3-319-81624-1978-3-319-33882-8
26#
發(fā)表于 2025-3-26 03:21:01 | 只看該作者
Yurii Galushkinerenden Folge wachsen. Ist die Beobachtungsfunktion durch nicht?quidistante Ordinaten belegt, so empfiehlt es sich, durch Interpolation (eventuell graphisch) eine gleichabst?ndige Folge herzustellen, was immer m?glich ist, wenn die gegebenen Werte überall dicht genug liegen. (Bezüglich lückenhafter Reihen verweise ich auf GuM S. 158f.)
27#
發(fā)表于 2025-3-26 08:04:40 | 只看該作者
28#
發(fā)表于 2025-3-26 09:24:52 | 只看該作者
29#
發(fā)表于 2025-3-26 14:08:24 | 只看該作者
Thermal Activation and Stretching of the East Barents Sea Lithosphere, Russia Barents Depression). According to the modeling, liquid hydrocarbons generated by the Ordovician, Silurian and Devonian deposits in the Admiralteyskoe Rise and by Devonian, Permian and considerable part of Triassic rocks in the South Barents depression were subjected (perhaps, partly) to secondary c
30#
發(fā)表于 2025-3-26 19:55:28 | 只看該作者
Thermal Regime and Extension of the Lithosphere in Different Tectonic Structures of the Sirte Basin,atform. Such a regime is caused mainly by the thermal activation of the lithosphere during the last 10?Ma. The intensity of this activation is highest in the western part of the Basin, where it is accompanied by the highest erosion amplitudes. The analysis of the variations in the basin tectonic sub
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