absorbed
发表于 2025-3-25 05:12:07
https://doi.org/10.1007/978-3-476-03388-8ts subsidence..Miocene-Pleistocene complex above the pre-Miocene unconformity continues from the Chukchi Basin to the Chukchi Plateau and marks the end of formation of these present-day morphological structures.
Mendicant
发表于 2025-3-25 07:55:02
http://reply.papertrans.cn/39/3834/383307/383307_22.png
neologism
发表于 2025-3-25 14:53:53
Lyrik in der DDR und die Moderne, that the basin did not form by a simple rift/extension scenario, but rather more likely through a complexity of events that included variably oriented extension, trans-tension and transform tectonics. Additionally, emplacement of the high arctic magnetic domain (Alpha Ridge and Mendeleev Rise) mask
恭维
发表于 2025-3-25 17:11:14
http://reply.papertrans.cn/39/3834/383307/383307_24.png
carotid-bruit
发表于 2025-3-25 21:16:22
Chukchi Plateau and Chukchi Basin,ts subsidence..Miocene-Pleistocene complex above the pre-Miocene unconformity continues from the Chukchi Basin to the Chukchi Plateau and marks the end of formation of these present-day morphological structures.
反话
发表于 2025-3-26 00:45:19
Extensional Structures of the Central Arctic Uplifts Complex,erpreted as relicts of the pre-oceanic Ellesmerian structural stage preserved in near-shelf tectonic depressions. They are strongly affected by rifting only at the elevated parts of the Central Arctic Uplifts Complex, and much less – in the depocenters of the sedimentary depressions.
Consequence
发表于 2025-3-26 05:25:47
Canada Basin, that the basin did not form by a simple rift/extension scenario, but rather more likely through a complexity of events that included variably oriented extension, trans-tension and transform tectonics. Additionally, emplacement of the high arctic magnetic domain (Alpha Ridge and Mendeleev Rise) mask
INERT
发表于 2025-3-26 10:50:47
http://reply.papertrans.cn/39/3834/383307/383307_28.png
CURT
发表于 2025-3-26 16:01:00
http://reply.papertrans.cn/39/3834/383307/383307_29.png
焦虑
发表于 2025-3-26 17:44:23
Seismic Stratigraphy of Sedimentary Cover,re dated either by well data (ACEX IODP 302 on the Lomonosov Ridge), or by correlation of their onlaps on acoustic basement with the nearest identifiable linear magnetic anomaly..The interpretation of pre-Cenozoic stratigraphy in the Central Arctic Uplifts Complex (CAUC) was based on tracing several