造山带地区花岗岩类构造混杂现象研究——以清水泉地区为例

STUDY OF THE TECTONIC INTERLARD PHENOMENA OF GRANITOIDS IN OROGENIC AREA:EXAMPLED BY QINGSHUIQUAN AREA,QINGHAI PROVINCE

通过对东昆仑东段清水泉地区花岗岩类的详细野外研究，提出造山带地区岩浆岩中普遍存在构造混杂现象，并把构造混杂岩浆岩分为构造岩浆岩片和准构造岩浆岩片两类，为造山带地区侵入岩的研究提供了新思路。

Based on the detail field study of granitoids of Qingshuiquan area in the east part of East Kunlun area,tectonic interlard phenomena is supposed to be ubiquitous in orogenic area and the tectonic interlard magmatic rocks is divided into two types:tectono magmatic slice and quasi tectono magmatic slice.