海南岛二叠纪沉积物成因转换对东古特提斯洋关闭的响应

IF 1.2 4区地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY

Australian Journal of Earth Sciences Pub Date : 2024-08-27 DOI:10.1080/08120099.2024.2389473

Z. J. Xu, S. Y. Gao, J. T. Kong, R. H. Cheng

引用次数: 0

摘要

二叠纪晚期至三叠纪早期，古特提斯洋东部封闭，长江克拉通与印度支那克拉通之间形成了金沙江-老山-宋马缝合带。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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Response of Permian sediment provenance conversion in Hainan Island to the closure of the Eastern Paleo-Tethys Ocean

From the late Permian to Early Triassic, the eastern part of the Paleo-Tethys Ocean was closed, and the Jinshajiang–Ailaoshan–Songma suture belt formed between the Yangtze Craton and the Indochina ...

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来源期刊

Australian Journal of Earth Sciences 地学-地球科学综合

CiteScore

2.80

自引率

8.30%

发文量

审稿时长

6-12 weeks

期刊介绍： Australian Journal of Earth Sciences publishes peer-reviewed research papers as well as significant review articles of general interest to geoscientists. The Journal covers the whole field of earth science including basin studies, regional geophysical studies and metallogeny. There is usually a thematic issue each year featuring a selection of papers on a particular area of earth science. Shorter papers are encouraged and are given priority in publication. Critical discussion of recently published papers is also encouraged.