Mutter 发表于 2025-3-30 10:12:21
http://reply.papertrans.cn/19/1810/180938/180938_51.png疯狂 发表于 2025-3-30 15:13:03
http://reply.papertrans.cn/19/1810/180938/180938_52.pngcinder 发表于 2025-3-30 19:27:20
http://reply.papertrans.cn/19/1810/180938/180938_53.png暴发户 发表于 2025-3-30 21:51:33
Tectonic Evolution of Northwestern South America “rift and drift” phases of the breakup of Pangea. During latest Cretaceous and into the Paleocene, microplate collision affected the entire South American margin, locally forming a suture. Interactions with the Caribbean and Nazca plates intensified and, starting in Miocene time with a Pliocene peaUrea508 发表于 2025-3-31 01:23:50
http://reply.papertrans.cn/19/1810/180938/180938_55.pngAmbiguous 发表于 2025-3-31 07:43:32
http://reply.papertrans.cn/19/1810/180938/180938_56.pngprostatitis 发表于 2025-3-31 12:54:43
http://reply.papertrans.cn/19/1810/180938/180938_57.png小步舞 发表于 2025-3-31 14:55:03
Fundamental Crustal Lineaments and Transverse Structural Zones in Continental Rifts as kinematic analogues of oceanic transform faults. However, detailed seismic interpretation and structural mapping of transverse zones in the North Sea Rift have revealed a connection between the transverse zones and fundamental basement lineaments in N.W. Europe. Major offsets of the Mesozoic Nor高贵领导 发表于 2025-3-31 19:44:02
Tectonic Controls on the Lake Victoria Basinund the craton margins, and intersection among a series of NW-trending strike-slip faults which transect the craton. Casual observation might suggest that the basin was formed by meteorite impact (Saul and Glaholm, 1981), but there is no geologic evidence (i.e., impact breccias, tektites, radial fra最高点 发表于 2025-3-31 22:13:21
Basement Extension on the Newfoundland Continental Margin (Canadian East Coast)ower crustal zone and underlies most of the Newfoundland offshore structural elements. A linked system of synthetic and antithetic faults associated with this crustal detachment now borders the structural units of the shelf..The widespread reactivation of pre-existing Precambrian and Paleozoic zones