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关注:1
2013-05-23 12:21
求翻译:早二叠至晚二叠世早期地壳沉降,海水浸漫,晚二叠世晚期海退为陆相沉积,形成与地槽完全不同的陆海陆相(C3-P)沉积。晚二叠世末-早三叠世地壳抬升,伴有断裂和安山岩喷发,早三叠世的陆相杂色堆积,标志着陆缘活动结束。由于印支运动强烈导致地块晚三叠世的卷入陆内造山,花岗岩侵入是什么意思? 待解决
悬赏分:1
- 离问题结束还有
早二叠至晚二叠世早期地壳沉降,海水浸漫,晚二叠世晚期海退为陆相沉积,形成与地槽完全不同的陆海陆相(C3-P)沉积。晚二叠世末-早三叠世地壳抬升,伴有断裂和安山岩喷发,早三叠世的陆相杂色堆积,标志着陆缘活动结束。由于印支运动强烈导致地块晚三叠世的卷入陆内造山,花岗岩侵入
问题补充: |
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2013-05-23 12:21:38
Early Permian to Late Permian to early crustal subsidence, sea flooding diffuse, Late Permian sea retreat continental deposits, the formation of the geosyncline completely different land and sea, continental (c3,-p) deposition. The end of the Late Permian - Early Triassic crustal uplift, accompanied
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2013-05-23 12:23:18
As early as 2 nights 2 stack up to the early settlement, crustal water flooding spread 2 stack, and the late night sea and land to the sediment, and completely different from slots to the land, sea, air and land (C P) 3 - sediment. Stack 2 nights end - the Earth's crust as early as 3 stack lift, acc
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2013-05-23 12:24:58
The early permian no later than the permian world early time earth's crust subsidence, the sea water immersion inundates, the late permian world later period regression is the continental deposit, forms with the geosyncline completely different land sea land facies (C3-P) deposition.The late permian
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2013-05-23 12:26:38
Early Permian to the early late Permian crustal subsidence, sea water immersion diffuse, late late Permian sea back to continental sedimentation, geosynclin e, totally different from land, sea and the formation of continental (C3-P) deposits. End of late Permian-early Triassic crustal uplift, accomp
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2013-05-23 12:28:18
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