辽西医巫闾山地区中、晚侏罗世地壳伸展作用的特征
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摘要
医巫闾山地区位于华北克拉通北缘,燕山山脉东段,区内广泛发育的太古宙深变质岩以及区内的变质核杂岩和伸展盆地,为研究岩石圈的流变学特点和华北克拉通的破坏提供了素材,从而引起了地质学者的关注。本文根据区内韧性剪切带及花岗岩体和岩脉的变形特点,确定医巫闾山地区中生代花岗岩体及岩脉为同伸展侵位。同构造岩脉的SHRIMP年代学研究及其它年代学资料显示:医巫闾山地区发生过两期伸展变形,分别发生在中、晚侏罗世和早白垩世。剪切带内的构造要素、岩石显微组构及矿物优选方位显示:早期伸展作用方向为SW,形成于中、下地壳的中、高温环境,表现为较低的应力和低应变速率下的高温韧性变形;晚期伸展作用方向为NWW,形成于上地壳的中、低温环境,表现为高应变速率下的低温韧、脆性变形。区内中、晚侏罗世伸展变形的厘定,表明华北克拉通的破坏在燕山早期已经开始,中、晚侏罗世太平洋构造域的影响使华北东部形成了挤压与伸展共存的构造格局。
In recent years, lithosphere thinning and destruction of the North China Craton are intensively discussed. Extensional crustal detachment is the most important tectonic response of lithosphere thinning and Yiwulümetamorphic core complex is useful to research destruction of the North China Craton. Although a great many achievements about the geological structure and granite in Yiwulüshan area have been made, there are still some puzzles and arguments. This paper study the Mesozoic geological structure in Yiwulüshan area through field geological investigation, microstructure, lattice preferred orientations and SHEIMP geochronology. The results are as follows:
①Extensional crenulation cleavage, rodding structure and“L”tectonite in the ductile shear zone and previous view show that its extensional shear zone. The ductile shear zone in Yiwulüshan area has composed with two department: Waziyu ductile shear zone and Yiwulüshan ductile shear zone. The former is dominated by low-temperature ductile deformation and the latter dominated by high-temperature tenacity deformation.
②Yiwulüshan ductile shear zone deformed in the early and Waziyu ductile shear zone derormed in the late, the fabric deformed at low temperature transformed from the high-temperature fabric. Early extension is in the direction of 220°~136°, the direction of the late extension is 270°~290°. Angle between the direction of two stages extension is about 30°~60°.
③Emplacement of Mesozoic granite in research area is controlled by C and S foliation of ductile shear zone and the mylonitic foliation in granite coordinates to it in wall rock, witch implies the granitic pluton and dikes emplacement as syn-tectonic granite. The pluton emplace along or parallel to ductile shear zone as a bedding-sill, based on the deformation character of granite and structure zone in Yiwulüshan region. SHRIMP geochronology of the syn-extensional granite dike provides it emplaced at 155±2Ma, combine with previous data shows crustal extension occurred in Yiwulü-shan region in middle-late Jurassic and early Cretaceous.
④Microstructure and lattice preferred orientations of quartz in Yiwulüshan ductile shear zone implies that deformation temperature of early extension is 550℃~ 700℃, deformed at high temperature environment in the middle and lower crust. Analysis of dynamically recrystallised grain size shows the differential stress of early extension is 9.6~13.9Mpa, deformation of the rock mainly as mineral plastic flow under high temperature.
⑤Redefinition of Yiwulüshan region middle-late Jurassic extension in implies that the Yanshan region and western Liaoning Province in the extension system from late Middle Jurassic to early Late Jurassic, destruction of the North China Craton has already begun at middle Jurassic, eastern of North China has become subject to the control of the Pacific tectonic domain and become the tectonic framework both compress and extension.
In recent years, lithosphere thinning and destruction of the North China Craton are intensively discussed. Extensional crustal detachment is the most important tectonic response of lithosphere thinning and Yiwulümetamorphic core complex is useful to research destruction of the North China Craton. Although a great many achievements about the geological structure and granite in Yiwulüshan area have been made, there are still some puzzles and arguments. This paper study the Mesozoic geological structure in Yiwulüshan area through field geological investigation, microstructure, lattice preferred orientations and SHEIMP geochronology. The results are as follows:
①Extensional crenulation cleavage, rodding structure and“L”tectonite in the ductile shear zone and previous view show that its extensional shear zone. The ductile shear zone in Yiwulüshan area has composed with two department: Waziyu ductile shear zone and Yiwulüshan ductile shear zone. The former is dominated by low-temperature ductile deformation and the latter dominated by high-temperature tenacity deformation.
②Yiwulüshan ductile shear zone deformed in the early and Waziyu ductile shear zone derormed in the late, the fabric deformed at low temperature transformed from the high-temperature fabric. Early extension is in the direction of 220°~136°, the direction of the late extension is 270°~290°. Angle between the direction of two stages extension is about 30°~60°.
③Emplacement of Mesozoic granite in research area is controlled by C and S foliation of ductile shear zone and the mylonitic foliation in granite coordinates to it in wall rock, witch implies the granitic pluton and dikes emplacement as syn-tectonic granite. The pluton emplace along or parallel to ductile shear zone as a bedding-sill, based on the deformation character of granite and structure zone in Yiwulüshan region. SHRIMP geochronology of the syn-extensional granite dike provides it emplaced at 155±2Ma, combine with previous data shows crustal extension occurred in Yiwulü-shan region in middle-late Jurassic and early Cretaceous.
④Microstructure and lattice preferred orientations of quartz in Yiwulüshan ductile shear zone implies that deformation temperature of early extension is 550℃~ 700℃, deformed at high temperature environment in the middle and lower crust. Analysis of dynamically recrystallised grain size shows the differential stress of early extension is 9.6~13.9Mpa, deformation of the rock mainly as mineral plastic flow under high temperature.
⑤Redefinition of Yiwulüshan region middle-late Jurassic extension in implies that the Yanshan region and western Liaoning Province in the extension system from late Middle Jurassic to early Late Jurassic, destruction of the North China Craton has already begun at middle Jurassic, eastern of North China has become subject to the control of the Pacific tectonic domain and become the tectonic framework both compress and extension.
引文
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[5]邓晋福,苏尚国,刘翠,等.关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论:是拆沉,还是热侵蚀和化学交代?[J]地学前缘, 2006, 13(2): 105-119.
[6]邓晋福,莫宣学,赵海玲.中国东部岩石圈根/去根作用与大陆“活化”-东亚型大陆动力学模式研究,现代地质, 1994, 8(3): 349-356.
[7]邓晋福,苏尚国,赵海玲,等.华北地区燕山期岩石圈减薄的深部过程[J].地学前缘, 2003, 10(3): 41-50.
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[9]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘, 2002, 10(3): 51-60.
[10]吴福元,徐义刚,高山,等.华北岩石圈减薄与克拉通破坏研究的主要学术争论[J].岩石学报, 2008, 24(6): 1145-1174.
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