西秦岭天水地区"李子园群"的解体及其构造环境浅析

修回日期: 2004-01-02

刊出日期: 2004-12-15

Analysis of the disintegration and tectonic setting of the "Liziyuan Group" in the Tianshui area, western Qinling

Revised Date: 02 January 2004

Publish Date: 15 December 2004

摘要: 依据岩石组成及变质变形特征,西秦岭天水地区“李子园群”可解体为5部分。初步研究认为,关子镇蛇绿岩形成于洋盆环境;流水沟变质中基性杂岩体为加里东期岛弧型深成杂岩体;李子园群(狭义)形成于北秦岭南缘弧前盆地环境;太阳寺岩组形成于扬子板块北缘被动陆缘环境;舒家坝群上部灰岩组形成于西秦岭微板块北缘半深海—深海盆地环境。
- 李子园群 /
- 蛇绿岩 /
- 太阳寺岩组 /
- 天水地区 /
- 西秦岭
Abstract: The "Liziyuan Group" in the Tianshui area, western Qinling, can be disintegrated into five parts according to its composition and metamorphic and deformation features. By field survey and study, the authors have the following ideas: the Guanzizhen ophioli
- Liziyuan Group /
- ophiolite /
- Taiyangsi Formation /
- Tianshui area /
- West Qinling