Výsledky vyhledávání - "Biete, Cristina"

Akademický článek

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Three-dimensional structure of the southwest Taiwan fold-and-thrust belt on the outer shelf and slope of the Eurasian margin

Autor: Alvarez-Marrón, Joaquina, Biete, Cristina, Brown, Dennis, Kuo-Chen, Hao

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
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The southwest Taiwan fold-and-thrust belt is forming on the outer shelf and slope of the Eurasian continental margin. It comprises a roughly N-S striking, west-verging imbricate thrust system that has been developing since the Late Miocene. Here, we

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c0ff8ddde18b46871205aa2dbd6b866f
http://hdl.handle.net/10261/180089

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Spatial distribution of the horizontal stress in the fold-and-thrust belt of south-central Taiwan from earthquake focal mechanisms

Autor: Biete, Cristina, Lund, B., Brown, Dennis, Alvarez-Marrón, Joaquina, Wu, Y. M., Kuo-Chen, Hao, Ho, Chun-Wei

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
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Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c49b79552f53bc671fdb456b21403cfb
http://hdl.handle.net/10261/189907

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How the structural architecture of the Eurasian continental margin affects the structure, seismicity, and topography of the south central Taiwan fold-and-thrust belt

Autor: Brown, Dennis, Alvarez-Marrón, Joaquina, Biete, Cristina, Kuo-Chen, Hao, Camanni, Giovanni, Ho, Chun-Wei

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
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Studies of mountain belts worldwide show that along-strike changes are common in their foreland fold-and-thrust belts. These are typically caused by processes related to fault reactivation and/or fault focusing along changes in sedimentary sequences.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::8f3bb5e94f38842cd65fddca642b3971
http://hdl.handle.net/10261/153508

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The structure of the south Taiwan fold-and-thrust belt

Autor: Biete, Cristina, Alvarez-Marrón, Joaquina, Brown, Dennis, Kuo-Chen, Hao, Ho, Chun-Wei

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
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The structure of the south Taiwan fold-and-thrust belt (FTB) comprises a roughly N-S striking, west-verging imbricate thrust system that has been developing since the Late Miocene. Here, we present the results of new surface geological mapping, seria

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::d305f0413e03c9ec6d3ae7da5658feba
http://hdl.handle.net/10261/162811

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Akademický článek

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Along-strike changes in the structure, seismicity, and topography of the south-central Taiwan fold-and-thrust belt inherited from the Eurasian margin

Autor: Brown, Dennis, Alvarez-Marrón, Joaquina, Biete, Cristina, Kuo-Chen, Hao, Camanni, Giovanni, Ho, Chun-Wei

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
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Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::9981719c9b1f504c2f52cefa1b88c7d3
http://hdl.handle.net/10261/163071

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'Diapiric architecture controlled by syn- and post-extension prograding sedimentary wedges'. ICTJA Student Presentation Award 2016

Autor: Moragas, Mar, Kumar, Ajay, Andrés, Juvenal, Peral, M., Sánchez-Pastor, Pilar, Biete, Cristina

Why rocks are not always deformed in the same way? How mountain chains are formed? Why rivers are distributed in specific patterns in a mountain region? How the plate tectonics are deformed in a subduction boundary? Some geological processes are diff

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______1106::0493045463b0ceecc9d6731ed5d004c3
http://hdl.handle.net/10261/237768

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Reactivation of Inherited Oblique Continental Margin Structures During the Development of the South-Central Taiwan Fold and Thrust Belt

Autor: Biete, Cristina, Alvarez-Marrón, Joaquina, Brown, Dennis, Kuochen, H., Ho, Chun-Wei, Wu, Y. M.

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
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The Taiwan orogen is forming due to the oblique collision between the Eurasian continental margin and the Luzon Arc. This configuration provides an opportunity to study the effect of inherited structures on the development of a fold and thrust belt (

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c78909948f71ed5c6619028e926e7047
http://hdl.handle.net/10261/163828

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