砍伐
发表于 2025-3-25 06:17:35
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.
crumble
发表于 2025-3-25 11:00:28
http://reply.papertrans.cn/67/6672/667145/667145_22.png
缺陷
发表于 2025-3-25 15:02:16
http://reply.papertrans.cn/67/6672/667145/667145_23.png
ciliary-body
发表于 2025-3-25 17:13:38
http://reply.papertrans.cn/67/6672/667145/667145_24.png
Flounder
发表于 2025-3-25 21:29:13
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
运动吧
发表于 2025-3-26 03:21:01
Yurii Galushkinerenden Folge wachsen. Ist die Beobachtungsfunktion durch nichtäquidistante Ordinaten belegt, so empfiehlt es sich, durch Interpolation (eventuell graphisch) eine gleichabständige Folge herzustellen, was immer möglich ist, wenn die gegebenen Werte überall dicht genug liegen. (Bezüglich lückenhafter Reihen verweise ich auf GuM S. 158f.)
值得
发表于 2025-3-26 08:04:40
http://reply.papertrans.cn/67/6672/667145/667145_27.png
inclusive
发表于 2025-3-26 09:24:52
http://reply.papertrans.cn/67/6672/667145/667145_28.png
清楚
发表于 2025-3-26 14:08:24
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
Acetaldehyde
发表于 2025-3-26 19:55:28
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