隼鹰 发表于 2025-3-26 23:15:34
https://doi.org/10.1007/978-3-642-28006-1s are examined successively along the southern, western and northern boundaries of the basin. Each site visited documents key successions of fault movements, continental clastic influx, marine sedimentation, or landscape change in the surrounding uplands as a result of widespread extensional tectoni退出可食用 发表于 2025-3-27 01:23:49
http://reply.papertrans.cn/39/3834/383373/383373_32.png慌张 发表于 2025-3-27 05:45:44
http://reply.papertrans.cn/39/3834/383373/383373_33.pngDEBT 发表于 2025-3-27 13:10:16
http://reply.papertrans.cn/39/3834/383373/383373_34.png摇曳的微光 发表于 2025-3-27 13:56:23
http://reply.papertrans.cn/39/3834/383373/383373_35.png表状态 发表于 2025-3-27 21:43:09
Charles V. Pollack Jr.,Victoria G. Riese the sediment record contained in the more westerly basins of Cerdagne and Capcir, which exclusively display late Miocene stratigraphic sequences until now not encountered among the extensional basins of itineraries 1–6. Another highlight is the widespread population of erosion surfaces that eitherGustatory 发表于 2025-3-28 01:58:04
http://reply.papertrans.cn/39/3834/383373/383373_37.png热情赞扬 发表于 2025-3-28 06:01:28
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http://reply.papertrans.cn/39/3834/383373/383373_39.png流浪 发表于 2025-3-28 10:27:57
Differential Diagnosis of Fractureistocene glaciation among the surrounding massifs. Late Pleistocene and older glacial landforms and deposits are particularly well documented because sequences of moraines and glacifluvial terraces are well preserved across the Cerdagne Basin floor.