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将东昆仑造山带划分为东昆北古老基底单元、东昆中早古生代构造混杂岩带、东昆南早古生代构造混杂岩带、马尔争-布青山晚古生代构造混杂岩带和巴颜喀拉山三叠纪浊积盆地5个次级构造单元,重新厘定了东昆仑不同构造混杂岩带的组成、结构、性质和时代,恢复了古海盆的演化历史。通过成分分析和颗粒裂变径迹年龄分析,确定了测区巴颜喀拉山群物源来自北部,基底性质可与马尔争-布青山带相对比,恢复了巴颜喀拉山群经历的构造热历史。运用构造年代学分析方法限定了测区经历的几次重大地质历史转折事件。确定了测区浆混花岗岩的存在。通过构造地貌和第四纪沉积分析,揭示了测区第四纪成山作用过程、水系变迁过程和古环境古气候演变过程。新发现一中型砂岩型铜矿。
The East Kunlun orogenic belt is divided into the ancient base unit of East Kunqun, the Mesozoic Early-Mesozoic tectonic melange belt in East Kunming, the Early Quaternary tectonic melange belt in East Kunlun, the Late Paleozoic tectonic melange belt in the Mar- The five sub-tectonic units in the Triassic turbidite basin re-determine the composition, structure, properties and times of the different structural melange belts in East Kunlun and restore the evolution history of the ancient sea basin. By means of composition analysis and fission track age analysis, it is confirmed that the source of the Bayan Har Mountains in the survey area is from the north, and the nature of the basement can be compared with that of the Marbian-Buqingshan zone and the structure experienced by the Bayan Har Mountains Hot History. Tectonic geochronology is used to define several major geological and historical turning events in the survey area. Confirmed the presence of mud zone mixed granite. Through the analysis of tectonic geomorphology and Quaternary sedimentary analysis, the process of Quaternary mountain formation, the evolution of water system and paleoclimate paleoclimate evolution are revealed. A new medium-sized sandstone-type copper deposit was discovered.