意见一致 发表于 2025-3-25 06:39:11
http://reply.papertrans.cn/63/6235/623446/623446_21.png疲劳 发表于 2025-3-25 10:16:27
http://reply.papertrans.cn/63/6235/623446/623446_22.pngForegery 发表于 2025-3-25 13:20:23
http://reply.papertrans.cn/63/6235/623446/623446_23.png时间等 发表于 2025-3-25 19:10:50
http://reply.papertrans.cn/63/6235/623446/623446_24.png浮雕 发表于 2025-3-25 21:16:58
http://reply.papertrans.cn/63/6235/623446/623446_25.pngabduction 发表于 2025-3-26 01:58:57
http://reply.papertrans.cn/63/6235/623446/623446_26.png轻浮思想 发表于 2025-3-26 06:35:39
http://reply.papertrans.cn/63/6235/623446/623446_27.pngMercantile 发表于 2025-3-26 11:19:04
Plastic Deformation of Gabbros in a Slow-spreading Mesozoic Ridge: Example of the Montgenèvre Ophiolelting within the sheared gabbros, at temperatures of 850° C or higher, generated augite- and pargasite-bearing leucodioritic magmas which evolved in narrow magmatic conduits and percolated through tec-tonites and actively deforming mylonite zones, to form cross-cutting veins in adjacent less deform使纠缠 发表于 2025-3-26 13:42:58
Pre-orogenic High Temperature Shear Zones in an Ophiolite Complex (Bracco Massif, Northern Apennines type 3). Reconstruction of the shear zones into their presumed original orientations suggests that they developed as low- to medium-angle extensional fault zones. This has important implications for the inferred processes of ophiolite generation.Nutrient 发表于 2025-3-26 18:44:13
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