The Ertix gold belt is located on the boundary of the Kalatongkearc and the Kelan back-arc basin of D-C1. Most scholars used to interpret the formation and distribution of the gold deposits in the Ertix tectonic belt ...The Ertix gold belt is located on the boundary of the Kalatongkearc and the Kelan back-arc basin of D-C1. Most scholars used to interpret the formation and distribution of the gold deposits in the Ertix tectonic belt in terms of the petrogenic and metallogenic models for active continental margins. However, enormous data of isotopic dating and geologic research show that the mineralization was obviously later than the oceanic subduction, whereas exactly simultaneous with the collisional orogenesis during C2-P, especially at the transition stage from collisional compression to extension. Based on study of metallogenic time, tectonic background, ore geology, ore fluid nature, ore material source, etc., we reveal that all the gold deposits possess the character of orogenic deposits formed in collisional orogenic system, and that their ore-forming materials mainly have derived from the stratigraphic terranes south to individual deposits. Accordingly, the theoretical tectonic model for collisional metallogenesis and petrogenesis is employed to explain the formation of the Ertix gold belt and to determine the gold exploration directions.展开更多
根据线粒体12S r RNA基因和S7核糖体蛋白基因内含子1序列,构建额尔齐斯河中11种鲤科鱼类的系统发育树。结果表明:12S基因AT含量与GC含量相当,而S7基因AT含量明显高于GC含量。12S基因保守区分散在整个序列中,而S7基因保守区均集中在前30...根据线粒体12S r RNA基因和S7核糖体蛋白基因内含子1序列,构建额尔齐斯河中11种鲤科鱼类的系统发育树。结果表明:12S基因AT含量与GC含量相当,而S7基因AT含量明显高于GC含量。12S基因保守区分散在整个序列中,而S7基因保守区均集中在前300bp内。12S r RNA和S7基因系统发育树中有三枝聚在一起,即贝加尔雅罗鱼Leuciscus baicalensis与高体雅罗鱼Leuciscus idus,尖鳍鮈Gobio gobio与麦穗鱼Pseudorasbora parva,金鲫Carassius carassius、银鲫Carassius auratus和鲤Cyprinus carpio。12S基因的聚类树中,丁鱥Tinca tinca与雅罗鱼亚科鱼类聚类,表明两者关系密切;而S7基因的聚类树中丁鱥以较高的支持率与尖鳍鮈、麦穗鱼聚在一起,与鮈亚科关系紧密;分子证据支持将丁鱥列入雅罗鱼系。12S基因构建的三种系统发育树拓扑结构有一定差异,而S7基因构建的三种系统发育树基本一致,支持率也高于前者,表明S7构建鲤科系统发育树的优势高于12S。展开更多
基金The authors thank Professors Tu Guangchi, Xiao Xuchang, He Guoqi, Ai Yongfu, Qin Kezhang and Wei QiyingDoctors Zhang Zengjie, Zhang Jing and Li Chao for their kindest help This work was supported by the Ministry of Science and Technology of China (Gr
文摘The Ertix gold belt is located on the boundary of the Kalatongkearc and the Kelan back-arc basin of D-C1. Most scholars used to interpret the formation and distribution of the gold deposits in the Ertix tectonic belt in terms of the petrogenic and metallogenic models for active continental margins. However, enormous data of isotopic dating and geologic research show that the mineralization was obviously later than the oceanic subduction, whereas exactly simultaneous with the collisional orogenesis during C2-P, especially at the transition stage from collisional compression to extension. Based on study of metallogenic time, tectonic background, ore geology, ore fluid nature, ore material source, etc., we reveal that all the gold deposits possess the character of orogenic deposits formed in collisional orogenic system, and that their ore-forming materials mainly have derived from the stratigraphic terranes south to individual deposits. Accordingly, the theoretical tectonic model for collisional metallogenesis and petrogenesis is employed to explain the formation of the Ertix gold belt and to determine the gold exploration directions.
