南美洲安第斯山脉中部：构造-岩浆演化述评

IF 1.7 4区地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY

Journal of South American Earth Sciences Pub Date : 2025-03-27 DOI:10.1016/j.jsames.2025.105503

Daniel Bertin , Emilce Bustos , Pablo Grosse , Walter Báez

{"title":"南美洲安第斯山脉中部：构造-岩浆演化述评","authors":"Daniel Bertin , Emilce Bustos , Pablo Grosse , Walter Báez","doi":"10.1016/j.jsames.2025.105503","DOIUrl":null,"url":null,"abstract":"<div><div>The Central Andes is a long-lived orogenic belt along the western margin of South America that includes the Central Volcanic Zone and two long-lived flat-slab segments, encompassing more than 3500 km between ∼5 and 33°S. The Central Andes has been the place of several outstanding geological processes since at least the latest Triassic (∼200 Ma), with the main development of the orogen taking place during the Eocene-Oligocene (45-25 Ma). In this contribution, we review and discuss the processes that have shaped and defined the crustal architecture of the Central Andes. We particularly highlight the role played by shallowing-steepening subduction cycles in controlling the tectono-magmatic evolution of the orogen, track the location of the current deformation front and the distribution of the stress field, and identify the regions where future high-flux magmatic episodes are most likely.</div></div>","PeriodicalId":50047,"journal":{"name":"Journal of South American Earth Sciences","volume":"158 ","pages":"Article 105503"},"PeriodicalIF":1.7000,"publicationDate":"2025-03-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The Central Andes of South America: A review of its tectono-magmatic evolution\",\"authors\":\"Daniel Bertin , Emilce Bustos , Pablo Grosse , Walter Báez\",\"doi\":\"10.1016/j.jsames.2025.105503\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The Central Andes is a long-lived orogenic belt along the western margin of South America that includes the Central Volcanic Zone and two long-lived flat-slab segments, encompassing more than 3500 km between ∼5 and 33°S. The Central Andes has been the place of several outstanding geological processes since at least the latest Triassic (∼200 Ma), with the main development of the orogen taking place during the Eocene-Oligocene (45-25 Ma). In this contribution, we review and discuss the processes that have shaped and defined the crustal architecture of the Central Andes. We particularly highlight the role played by shallowing-steepening subduction cycles in controlling the tectono-magmatic evolution of the orogen, track the location of the current deformation front and the distribution of the stress field, and identify the regions where future high-flux magmatic episodes are most likely.</div></div>\",\"PeriodicalId\":50047,\"journal\":{\"name\":\"Journal of South American Earth Sciences\",\"volume\":\"158 \",\"pages\":\"Article 105503\"},\"PeriodicalIF\":1.7000,\"publicationDate\":\"2025-03-27\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of South American Earth Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0895981125001658\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of South American Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0895981125001658","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}

引用次数: 0

摘要

中安第斯山脉是沿着南美洲西部边缘的一个长期存在的造山带，包括中央火山区和两个长期存在的平板段，在~ 5到33°S之间的范围超过3500公里。至少从三叠纪晚期（~ 200 Ma）开始，安第斯山脉中部就发生了几次突出的地质作用，造山带的主要发育发生在始新世-渐新世（45-25 Ma）。在这篇文章中，我们回顾并讨论了形成和定义安第斯山脉中部地壳结构的过程。我们特别强调了浅变陡俯冲旋回在控制造山带构造-岩浆演化中的作用，跟踪了当前变形锋的位置和应力场的分布，并确定了未来最有可能发生高通量岩浆活动的区域。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

查看原文本刊更多论文

The Central Andes of South America: A review of its tectono-magmatic evolution

The Central Andes is a long-lived orogenic belt along the western margin of South America that includes the Central Volcanic Zone and two long-lived flat-slab segments, encompassing more than 3500 km between ∼5 and 33°S. The Central Andes has been the place of several outstanding geological processes since at least the latest Triassic (∼200 Ma), with the main development of the orogen taking place during the Eocene-Oligocene (45-25 Ma). In this contribution, we review and discuss the processes that have shaped and defined the crustal architecture of the Central Andes. We particularly highlight the role played by shallowing-steepening subduction cycles in controlling the tectono-magmatic evolution of the orogen, track the location of the current deformation front and the distribution of the stress field, and identify the regions where future high-flux magmatic episodes are most likely.

求助全文

通过发布文献求助，成功后即可免费获取论文全文。去求助

来源期刊

Journal of South American Earth Sciences 地学-地球科学综合

CiteScore

3.70

自引率

22.20%

发文量

364

审稿时长

6-12 weeks

期刊介绍： Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields: -Economic geology, metallogenesis and hydrocarbon genesis and reservoirs. -Geophysics, geochemistry, volcanology, igneous and metamorphic petrology. -Tectonics, neo- and seismotectonics and geodynamic modeling. -Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research. -Stratigraphy, sedimentology, structure and basin evolution. -Paleontology, paleoecology, paleoclimatology and Quaternary geology. New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.