SNEER
发表于 2025-3-23 10:02:38
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Triglyceride
发表于 2025-3-23 15:45:47
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贝雷帽
发表于 2025-3-23 20:45:45
Politics of Social Change in Ghanaean flat slab to a normal subduction segment (32°–36°S). This segment shows remarkable along-strike variations in topographic uplift, structural elevation, amount and rate of shortening, and crustal root geometry. In the flat-slab segment, high elevations, the development of several tectonic provinc
BOLUS
发表于 2025-3-24 00:45:19
tion, an extensional event in late Oligocene times affected the western section of the Late Cretaceous to Eocene fold and thrust belt. Late early Miocene contraction then constructed most of the eastern Andean slope as in sequence structures stacked in the frontal sector of the fold and thrust belt.
Jubilation
发表于 2025-3-24 05:41:15
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使害羞
发表于 2025-3-24 06:59:26
The Weaponization of Congressional Oversightllowed establishing a structural control for the main sedimentary packages that coexisted with Andean development. These structures affect Miocene strata at the eastern deformational front, indicating a last stage of development, although cooling ages suggest a Mid to Late Cretaceous exhumation of t
山羊
发表于 2025-3-24 12:17:15
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freight
发表于 2025-3-24 16:41:06
David W. Paul (freelance writer, faculty)this sector has not been addressed yet. A review of recent advances in different aspects of the Patagonian orogen and its related broken foreland system reveals a close relation between the evolution of both sectors. This enabled us to integrate them in an evolutionary model connecting tectonic even
关节炎
发表于 2025-3-24 21:05:35
https://doi.org/10.1007/978-981-4585-57-6climatic, magmatic, deformational, and sedimentary events. Three orogenic and magmatic cycles can be particularly related to processes in the subduction zone (1) Late Cretaceous closure of the Rocas Verdes marginal basin, (2) Paleogene collision of the Farallón-Aluk seismic ocean ridge, and (3) Mioc
POLYP
发表于 2025-3-25 01:46:01
Politics, Citizenship and Rightsensional and magmatic processes in the southernmost Andes developed in continuity with the Antarctic Peninsula. The Rocas Verdes back-arc oceanic basin opened during the Jurassic along the Patagonian–Fuegian margin, widening toward the south were it connected with the Weddell Sea. Jurassic volcanicl