inscribe 发表于 2025-3-23 13:20:55
The Trappean Complex of the Siberian Platformof the East Siberia platform. The modeling of thermal regime and maturation history of sedimentary basin of the Siberian Platform is conducted on the examples of two sedimentary sections: the Kuyumba-12 well in the Kamo swell containing six sills in sedimentary section and the Kiramkinskaya-1 well oMUT 发表于 2025-3-23 15:47:41
Duration of the Intrusion Formation and Its Relation to the Size of Thermal and Maturity Aureoles ofand host sedimentary rocks to generate hydrocarbons. Our study shows that a size of maturity aureoles of the single intrusions and trap complex decreases considerably with increase of duration of these complex is formation. So, the aureole size in for formation of the trap with total thickness of 10冥界三河 发表于 2025-3-23 20:30:37
http://reply.papertrans.cn/67/6672/667145/667145_13.pngPrologue 发表于 2025-3-24 02:15:09
Evolution of Permafrost and of Gas Hydrate Stability Zoneions in paleoclimate is taken into consideration beginning with the time of the basin initiation and including the past 3.4 Ma, when formation and degradation of permafrost were repeated many times. The use of real lithological composition of sedimentary rocks distinguishes this approach from previoharbinger 发表于 2025-3-24 05:26:31
Influence of Climate Variations on Rock Temperature and Heat Flow permafrost evolution during the Pliocene-Quaternary in the intra-continental and shelf sedimentary basins. The chapter examines as regions with modern areas of permafrost (Urengoy field in the West Siberian Basin and Kuyumba field in the Siberian Platform) as the basins where permafrost degraded 10小样他闲聊 发表于 2025-3-24 09:13:13
http://reply.papertrans.cn/67/6672/667145/667145_16.png场所 发表于 2025-3-24 14:29:25
http://reply.papertrans.cn/67/6672/667145/667145_17.pngCAND 发表于 2025-3-24 15:56:18
978-3-319-81624-1Springer International Publishing Switzerland 2016Affection 发表于 2025-3-24 22:58:44
http://reply.papertrans.cn/67/6672/667145/667145_19.pngcircumvent 发表于 2025-3-24 23:51:32
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