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康滇地盾在过去一直被认为是一个較典型的地盾。但是仔細分析康滇地盾的地质史以后,觉得无論从沉积厚度、岩浆活动或构造变动中,均可看出康滇地盾的活动性在三迭紀以后有显著的增强。由于康滇地盾上許多金属与非金属矿产的生成与此有密切关系,因此弄清康滇地盾在中生代的活动性,对普查找矿工作,无疑将有許多帮助。作者认为,康滇地盾在后期(中生代)有活化現象,其根据是: 一、断裂发育、部分地区的褶皺很强烈自会理至盐边,长达几公里至十几公里,甚至几十公里的断层,就有5—6条之多。在永仁那拉箐煤田和攀枝花矿区,除灰槽子逆断层及灰老张正断层外,沿攀枝花輝长岩体分布之地区,显然有一隐伏的基底断裂存
Kang Dian shield in the past has been considered as a more typical shield. However, after careful analysis of the geological history of the Kang-Dian Earthquake, we can see that the activity of the Kandian Shield increased significantly after Triassication in terms of sedimentary thickness, magmatic activity or structural changes. Because many metal and non-metallic minerals on Kangdi Dian Shield are closely related to the formation of this mineral, it is undoubtedly of great help to understand the activities of the Kangdi Dianlizu in Mesozoic during the Mesozoic era. The author believes that the Kangdian shield in the late (Mesozoic) there is an activation phenomenon, based on: First, the fracture development, in some parts of the fold is very strong from the Council to the salt side, up to a few kilometers to ten kilometers, or even dozens of Km fault, there are as many as 5-6. In the areas of Lajin Coalfield and Panzhihua Mining Area of Yongren, except the Grease Trench Reversal and the Gregor Chang Zhangzheng Fault, there is obviously a hidden basement fault deposit along the distribution of the Panzhihua gabbro body