地学前缘 ›› 2011, Vol. 18 ›› Issue (1): 1-8.

• 论文 •    下一篇

岩石成因与岩石圈演化思考

陈国能   

  1. 中山大学 地球科学系, 广东 广州 510275
  • 收稿日期:2010-10-16 修回日期:2010-11-28 出版日期:2011-01-15 发布日期:2011-01-15
  • 作者简介:陈国能(1952—),男,教授,主要研究方向为花岗岩成因与成矿、大地构造与新构造。Email: chengn@mail.sysu.edu.cn
  • 基金资助:

    高等学校博士学科点基金项目(20070558033);广东省自然科学基金重点项目(10251027501000019)

Pondering over the genesis of rocks and the evolution of lithosphere.

  1. Department of Earth Sciences, Sun YatSen University, Guangzhou 510275, China
  • Received:2010-10-16 Revised:2010-11-28 Online:2011-01-15 Published:2011-01-15

摘要:

岩石圈内能变化导致岩石的形成和消亡。组成岩石圈的三种不同类型岩石的形成和消亡过程在岩石圈表面引起不同的大地构造效应。大洋岩石圈和大陆岩石圈的演化效应存在互补关系:前者内能升高导致岩石形成,反之岩石消亡;后者内能升高导致岩石消亡,反之岩石形成;前者造成平、剖面上均自洋中脊向外变老的岩石序列,后者造成平面上自陆核向外变新,剖面上自重熔界面向上和向下变新的岩石序列。

关键词: 岩石成因, 大地构造效应, 岩石圈演化, 陆壳熔融

Abstract:

Variation of intrinsic energy of the lithosphere results in forming and perishing of rocks. Evolution of the three kinds of rocks that constitute the lithosphere produces different tectonic effects on the earth surface, and the evolutional effects on the oceanic and continental crusts are found with complementing relationship: increasing intrinsic energy in the oceanic lithosphere leads to the birth of rocks, otherwise to the perish; and in the continental lithosphere, increasing intrinsic energy leads to the perish of rocks, otherwise to the birth. The former process creates a rocksequence in which the rocks become older from the mid oceanic ridge outwards either on a horizontal plane or on a vertical section, and the latter produces a rocksequence in which the rocks become younger from the core of a continent outwards on a horizontal plane and become younger from the MI upwards and downwards on a vertical section.

Key words:  rock genesis, tectonic effect, evolution of lithosphere, crustal melting

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