The Deformation Age of Palaeozoic-Mesozoic Tectonic along North Xin-Zang Road in West Kunlun
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摘要: 为了建立西昆仑地区构造-热事件序列, 利用40Ar/39Ar同位素分析法对西昆仑新藏公路康西瓦断裂带以北具有代表性的同构造新生变质矿物角闪石、黑云母、绢云母单矿物进行了年龄测定, 得到几个多次出现的年龄值.结合早期该区发育的各类岩脉的侵位年龄综合分析, 认为片麻岩中单矿物黑云母440Ma和(403±6) Ma40Ar/39Ar年龄, 可代表早古生代俯冲变质年龄以及增生过程所持续的时间; 片岩、片麻岩中黑云母, 斜长角闪片岩(基性岩脉) 中单矿物角闪石的40Ar/39Ar年龄为382Ma~84Ma, 代表着该区从早古生代晚期的挤压构造环境转化为引张环境及其所持续的时间; 晚期脆性断裂中云母类矿物178Ma~65Ma的40Ar/39Ar年龄, 代表着该区在挤压走滑构造背景中断裂构造的脉冲式活动及其持续时间.
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关键词:
- 40Ar/39Ar定年 /
- 古生代 /
- 俯冲增生作用 /
- 西昆仑
Abstract: To establish the list of tectonic-metamorphic events in West Kunlun, we have dated tectonic metamorphic minerals such as amphibole, biotite and didrimit through 40Ar-39Ar isotopic analysis. We have gained several ages that occur many times. Combined with the emplacement age of dikes developed in this area earlier, the 440 Ma and (403±6) Ma 40Ar∕39Ar age of individual mineral biotite in gneiss can represent early Paleozoic underthrut curdle age and the period of accretional process; 382 Ma-284 Ma age of individual mineral biotite in schiefer gneiss and individual mineral amphibole in amphibolite-schist can represent the changing environment from extrusion to spread of this area in early Paleozoic era; 178 Ma-165 Ma 40Ar∕39Ar age of biotite in fragile fault can represent the spurt action of fault tectonic in the background of extrusion strike-slip tectonic and its duration.-
Key words:
- 40Ar-39Ar dating /
- Paleozoic /
- subduction-accretion process /
- Tethys /
- West Kunlun
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表 1 黑云母、角闪石40Ar/39Ar快中子活化法定年数据
Table 1. The40Ar/39Ar dating data of biotite and amphibole in NA fast neutron activation method
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