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一、前言 本文是在最近所获之地质、地物及钻探资料的基础上,並参考前人有关的岩相古地理成果写成的。其中主要的有:王爱民等(1980年)编制的北疆地区岩相与等厚图;新疆地质局区调大队地层组(1979—1982年)所作新疆寒武系—二叠系专著;新疆石油管理局准噶尔盆地勘探研究大队(1983年)成果图集;新疆石油局南疆会战指挥部地质所的最近成果报告和雍天寿同志的关於塔里木盆地岩相古地理研究成果(1980—1983年)。 不言而喻,新疆区域构造背景、基底性质以及构造运动方式等,乃是控制本区沉积
I. Preface This article is based on the recent geological, geophysical and drilling data and references to the predecessor’s related achievements in lithofacies paleology. The main ones are: the lithofacies and isopachograms of northern Xinjiang prepared by Wang Aimin et al. (1980); Xinjiang Cambrian-Permian monographs made by the Geological Brigade Geological Formation (1979-1982); Xinjiang Petroleum The results gallery of the Exploration and Research Brigade of the Junggar Basin (1983); the recent achievements report of the Geological Institute of the Xinjiang Naval Battlefield Command and the Commentary on the lithofacies paleogeography of the Tarim Basin (1980-1983) by Comrade Yong Tianshou. It goes without saying that the regional tectonic setting, basement and tectonic movement in Xinjiang are the means to control the sedimentation in this area