张艳妮;李荣西;刘海青;

• 1:长安大学地球科学与资源学院

摘要(Abstract)：

纤维状方解石脉作为同构造期流体活动产物,被认为是在超高压构造应力作用下形成的一种高压流体排泄的标型矿物,记录了构造变形过程中的流体特征。从基本概念出发,介绍了纤维状方解石脉和构造流体的基本特征、形成机理和环境条件等。以大巴山前陆构造发育的纤维状方解石脉为例,综述了纤维状方解石脉和构造流体的研究方法、思路、内容及其构造意义,强调了构造脉体在古应力场恢复和构造变化研究中的重要意义。

关键词(KeyWords)： 构造流体;纤维状方解石脉;流体地球化学;古构造应力恢复;大巴山前陆构造

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(41173055);; 中国地质调查局项目(1212011121117)

作者(Author): 张艳妮;李荣西;刘海青;

Email:

DOI:

参考文献(References)：

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