Arid
DOI10.1016/j.jsames.2020.102990
Exhumation and structural evolution of the high-elevation Malcante Range, Eastern Cordillera, NW Argentina
Payrola, Patricio; Zapata, Sebastian; Sobel, Edward R.; del Papa, Cecilia; Pingel, Heiko; Glodny, Johannes; Ledesma, Jonathan
通讯作者Payrola, P (corresponding author), Univ Nacl Salta, CONICET, Inst Bio & Geociencias NOA IBIGEO, Av Bolivia 5150, RA-4400 Salta, Argentina.
来源期刊JOURNAL OF SOUTH AMERICAN EARTH SCIENCES
ISSN0895-9811
EISSN1873-0647
出版年2021
卷号105
英文摘要As an integral part of the Eastern Cordillera, the fault-bounded Malcante mountain range (up to 5100 m) in the NW Argentine Andes (ca. 25 degrees S) is located in the transition between the arid Puna Plateau to the west and the humid broken foreland to the east. At this latitude, the topographic gradient of the eastern Andean margin forms an efficient orographic barrier that causes pronounced east-west rainfall and surface-process gradients. In this setting, the Malcante Range is an important, yet poorly studied structural high formed during the Cenozoic topographic growth of the Central Andes. In this study, we combine (a) detailed field observations, (b) a two-dimensional structural reconstruction, (c) apatite fission track and (U-Th-Sm)/He thermochronology of bedrock samples from a vertical transect across the western flank of the Malcante Range, and (d) inverse thermal modelling using QTQt software with the aim of deciphering the exhumation history of this mountain range. Field data indicate the presence of an angular unconformity between Cenozoic foreland deposits and older sedimentary strata, suggesting an initial episode of deformation during the middle-late Eocene, while our thermal model constrains the onset of exhumation at similar to 10 Ma. We suggest that exhumation was related to the unroofing of the easily erodible sedimentary cover, which prevented significant initial surface uplift. This may have changed as more resilient bedrock was exposed at 5 Ma according to the thermal model, promoting rapid rock uplift. In combination with published data, our thermochronology allows us to speculate on the existence of a zone of deformation concentrated in the area of the present-day Pasha (24.5 degrees S), Malcante (25 degrees S), and Agua de Castilla (25.4 degrees S) mountain ranges by ca. 10 Ma.
英文关键词Thermochronology Apatite fission track Apatite (U-Th)/He Mountain building Eastern cordillera NW Argentina
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000606803300001
WOS关键词MIDDLE EOCENE DEFORMATION ; TRACK ANNEALING KINETICS ; APATITE (U-TH)/HE ; NORTHWESTERN ARGENTINA ; ANGASTACO BASIN ; THRUST BELTS ; UPLIFT ; SEDIMENTATION ; VARIABILITY ; TECTONICS
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/348041
作者单位[Payrola, Patricio] Univ Nacl Salta, CONICET, Inst Bio & Geociencias NOA IBIGEO, Av Bolivia 5150, RA-4400 Salta, Argentina; [del Papa, Cecilia; Ledesma, Jonathan] Univ Nacl Cordoba, CONICET, CICTERRA FCEFyN, Av Velez Sarsfield,1611,X5016GCA, Cordoba, Argentina; [Sobel, Edward R.; Pingel, Heiko] Univ Potsdam, Inst Geowissensch, Karl Liebknecht Str 24-25, D-14476 Potsdam, Germany; [Zapata, Sebastian] Smithsonian Trop Res Inst, POB 0843-03092, Balboa, Ancon, Panama; [Zapata, Sebastian] Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Rolla, MO 65409 USA; [Glodny, Johannes] Deutsch GeoForschungsZentrum GFZ, Telegrafenberg, Helmholtz Zentrum Potsdam, D-14473 Potsdam, Germany
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GB/T 7714
Payrola, Patricio,Zapata, Sebastian,Sobel, Edward R.,et al. Exhumation and structural evolution of the high-elevation Malcante Range, Eastern Cordillera, NW Argentina[J],2021,105.
APA Payrola, Patricio.,Zapata, Sebastian.,Sobel, Edward R..,del Papa, Cecilia.,Pingel, Heiko.,...&Ledesma, Jonathan.(2021).Exhumation and structural evolution of the high-elevation Malcante Range, Eastern Cordillera, NW Argentina.JOURNAL OF SOUTH AMERICAN EARTH SCIENCES,105.
MLA Payrola, Patricio,et al."Exhumation and structural evolution of the high-elevation Malcante Range, Eastern Cordillera, NW Argentina".JOURNAL OF SOUTH AMERICAN EARTH SCIENCES 105(2021).
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