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作 者:张克信 黄继春 殷鸿福 王国灿 王永标 冯庆来 田军
机构地区:[1]China University of Geosciences, Wuhan 430074, China
出 处:《Science China Earth Sciences》2000年第4期364-374,共11页中国科学(地球科学英文版)
摘 要:The main character of melange strata in an erogenic belt is the integration of mixed materials due to the superposition, displacement or loss of various tectonic slices (blocks) of different origins and environments, different scales, different grades of deformation and metamor-phism, and different stages of tectonic evolution. The approach to non-Smith strata in an erogenic belt is to focus on the understanding of the age, facies, tectonic setting of the original formation and the process of deformation-metamorphism of each tectonic slice, reconstruct the history of dispersal and integration of these tectonic slices in time and space, i.e. 4-dimensional. This paper studies the age and facies of the original formation of tectonic slices in the A’nyemaqen melange belt based on new data of radiolarians, sporo-pollen and trace fossils, and cast new lights on the research of the evolution process of that belt.The main character of melange strata in an erogenic belt is the integration of mixed materials due to the superposition, displacement or loss of various tectonic slices (blocks) of different origins and environments, different scales, different grades of deformation and metamor-phism, and different stages of tectonic evolution. The approach to non-Smith strata in an erogenic belt is to focus on the understanding of the age, facies, tectonic setting of the original formation and the process of deformation-metamorphism of each tectonic slice, reconstruct the history of dispersal and integration of these tectonic slices in time and space, i.e. 4-dimensional. This paper studies the age and facies of the original formation of tectonic slices in the A'nyemaqen melange belt based on new data of radiolarians, sporo-pollen and trace fossils, and cast new lights on the research of the evolution process of that belt.
关 键 词:non-Smith STRATA radiolarian age fades East Kunlun orogenic belt.
分 类 号:Q915[天文地球—古生物学与地层学]
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