Structural style of the Chos Malal fold and thrust belt, Neuquén basin, Argentina: Relationship between thick- and thin-skinned tectonics
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- 作者：Natalia Sá ; ncheza ; natalia.sanchez@uns.edu.ar" class="auth_mail" title="E-mail the corresponding author ; Martí ; n Turienzoa ; turienzo@uns.edu.ar" class="auth_mail" title="E-mail the corresponding author ; Fernando Lebinsona ; fernando.lebinson@uns.edu.ar" class="auth_mail" title="E-mail the corresponding author ; Vanesa Araujoa ; vanesa.araujo@uns.edu.ar" class="auth_mail" title="E-mail the corresponding author ; Isabelle Coutandb ; icoutand@dal.ca" class="auth_mail" title="E-mail the corresponding author ; Luis Dimieria ; ldimieri@uns.edu.ar" class="auth_mail" title="E-mail the corresponding author
- 关键词：Thick-skinned structures ; Shortening ; Neuqué ; n basin ; Andean tectonics
- 刊名：Journal of South American Earth Sciences
- 出版年：2015
- 出版时间：December 2015
- 年：2015
- 卷：64
- 期：part_P2
- 页码：399-417
- 全文大小：13092 K
文摘
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Thick and thin-skinned structures characterize the Chos Malal FTB.
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Andean thrusts formed basement-involved wedges such as the Cordillera del Viento.
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First order basement wedges inserted in the cover produced second order folds.
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Structures in the cover combine fault-bend and fault-propagation folding mechanisms.