首页> 外文期刊>Acta geologica Sinica: Journal of the Geological Society of China >Three Stages of Mesozoic Bimodal Igneous Rocks and Their Tectonic Implications on the Continental Margin of Southeastern China
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Three Stages of Mesozoic Bimodal Igneous Rocks and Their Tectonic Implications on the Continental Margin of Southeastern China

机译:中国东南大陆边缘的中生代双峰火成岩的三个阶段及其构造意义

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摘要

There are large-scale Mesozoic bimodal igneous rock associations on the continental margin of southeastern China. They aroused extensive attention in the 1980s because of their specific tectonic implications, and have been found frequently during recent geological surveys. This paper reviews the studies of regional Mesozoic bimodal rocks, and concludes that they can be subdivided into three stages, i.e., the Early Jurassic (209-170 Ma, the first (I) stage), the Late Jurassic-early Early Cretaceous (154-121 Ma, the second (II) stage), and the late Early Cretaceous-Late Cretaceous (115-85 Ma, the third (III) stage). These three stages of bimodal rocks were formed in different tectonic settings, and are important indicators for regional Mesozoic tectonic evolution.
机译:中国东南部大陆边缘有大型中生代双峰火成岩组合。由于其特定的构造意义,它们在1980年代引起了广泛的关注,并且在最近的地质调查中经常发现。本文回顾了区域中生代双峰岩石的研究,并得出结论,它们可以分为三个阶段,即侏罗纪早期(209-170 Ma,第一(I)阶段),侏罗纪晚期-早白垩纪早期(154)。 -121 Ma,第二(II)阶段)和早白垩世-晚白垩世(115-85 Ma,第三(III)阶段)。这三个阶段的双峰岩形成于不同的构造环境中,是区域中生代构造演化的重要标志。

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