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書目名稱Growth of the Southern Andes影響因子(影響力)




書目名稱Growth of the Southern Andes影響因子(影響力)學(xué)科排名




書目名稱Growth of the Southern Andes網(wǎng)絡(luò)公開度




書目名稱Growth of the Southern Andes網(wǎng)絡(luò)公開度學(xué)科排名




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書目名稱Growth of the Southern Andes被引頻次學(xué)科排名




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書目名稱Growth of the Southern Andes年度引用學(xué)科排名




書目名稱Growth of the Southern Andes讀者反饋




書目名稱Growth of the Southern Andes讀者反饋學(xué)科排名

adipose-tissue

,Changes in Source Areas at Neuquén Basin: Mesozoic Evolution and Tectonic Setting Based on U–Pb Age we analyze the U–Pb zircon age database published for the Southern Central Andes. In the early Mesozoic (rift stage) the source regions were locally and strongly influenced by the active volcanism coeval with the extensional tectonic activity. The rift relief associated with the synrift stage laste

coagulation

,Cenozoic Orogenic Evolution of the Southern Central Andes (32–36°S),ean 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

insolence

,The Transitional Zone Between the Southern Central and Northern Patagonian Andes (36–39°S),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.

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reject

,Tectonic Evolution of the Northern Patagonian Andes (40°S),llowed 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

reject

,Cenozoic Deformational Processes in the North Patagonian Andes Between 40° and 43°S,al processes that acted through time and relate them to basin formation. Field observations and seismic reflection profiles reveal the shallow structure of the retroarc area where contractional structures, associated with Oligocene to early Miocene inverted extensional sections, are partially onlapp

Commodious

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,Growth of the Southern Patagonian Andes (46–53°S) and Their Relation to Subduction Processes,climatic, 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

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