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《Journal of Chengdu University of Technology(Science & Technology Edition)》 1986-02
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TECTONIC FEATURE OF GAIZE-SHUANGHU REGION, XIZANG (TIBET)

Huang Bangqiang  
Gaize--Shuanghu region is located at the northern part of Yunnan TibetGeosynclinal--folded Province, which includes three tectonic units of firstcategory, i.e., Songpan--Ganzi Folded System, Qiangtang Massif andKalakunlun Folded System. The northern part of the region is Kekexili Indo--China Foldbelt whichbelongs to the western extension of Songpan--Ganzi Folded System. LateHercynian--Indochinese basalts, basic--ultrabasic intrusives and blueschistsare widely distributed. Himalayan volcanic rocks are also observed. The central part of the region is Qiangtang Massif, whose presinianmetamorphic basement is overlain by middle Devonian--Jurassic marine sedimentsand late Yanshan--Himalayan continental sediments and volcanics. In thecentral area of the massif late Hercynian intermediate--basic volcanics andYeashan acidio intrusives are developed. Gaize--Dingqing Early Yenshanian Foldbelt is situated in the south of theregion and belongs to the eastern extension of Kalakunlun Folded System.EarlyYenshanian pillow layas, abyssal siliceous and basic--ultrabasic rocks are welldeveloped.During the late Yenshania period, volcanics and molasse formationsare formed at the north of the belt, while carbonate formation at the southof the belt.
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