北京云蒙山地区中生代岩浆活动及构造演化
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摘要
北京云蒙山地区位于华北克拉通北缘燕山褶断带中段。该地区发育大量中生代岩浆岩及近E—W向逆冲型四合堂剪切带和NE向伸展型大水峪剪切带。本次工作通过锆石年代学和单矿物(角闪石、黑云母)~(40)Ar/~(39)Ar年代学分析,进一步整理了云蒙山地区中生代岩浆活动及构造演化的时间,并分析了云蒙山岩基周边不同阶段的冷却速率。本次工作发现云蒙山地区经历了三期岩浆活动:晚三叠世、晚侏罗世和早白垩世。其中,206 Ma为捕获岩浆锆石年代学记录;在出露岩体中,沙陀子岩体为159~151 Ma,石城岩体为169~151 Ma,长园岩体为156~151 Ma,云蒙山岩基为146~141 Ma;冯家峪—西白莲峪花岗质岩体为130~124 Ma;冯家峪闪长质岩体为127 Ma;大东沟花岗质岩体为127 Ma。云蒙山地区经历了三次重要的构造事件。在早侏罗世,云蒙山地区表现为区域性角度不整合,并以挤压运动为主,缺乏岩浆活动。在早白垩世早期(143~135.5 Ma),云蒙山岩基北缘发育逆冲型四合堂剪切带。在早白垩世晚期(135~93.9 Ma),云蒙山地区发育以东南侧大水峪剪切带为主拆离剪切带的变质核杂岩。此外,云蒙山岩基的北侧和西侧,早期受四合堂剪切带影响,具有较高的冷却速率。云蒙山岩基的东侧,早期受四合堂剪切带影响较小,具有较小的冷却速率,以缓慢的均衡隆升为主,而晚期受大水峪剪切带强烈活动影响,为快速隆升阶段。总之,云蒙山地区在中生代经历了多期次的岩浆活动及构造运动,在不同地区呈现了阶段性不同程度的抬升剥蚀。
Objectives:Mount Yunmeng Area,Beijing locates in the middle part of Yanshan Orogeny,the northern margin of the North China Craton(NCC).In this area,there are many Mesozoic magmatic activities,the E—W-trending thrust Sihetang shear zone,and NE-trending extensional Dashuiyu shear zone.Although,many isotopic dating works have been done for these plutons and movements,there are less works to organize these data to describe their period relationship systematically and discuss their indication to the evolution of the Yunmengshan Metamorphic Core Complex(YMCC)and NCC.Methods:The zircon isotopic dating and single mineral(hornblende and biotite)~(40)Ar/~(39)Ar dating are analyzed in this work.The cooling rates around the Mount Yunmeng are calculated and discussed.Results:Through the Zircon U-Pb isotopic dating,the ages of plutons are defined.The 206 Ma comes from the trapped magma zircon.Among the exposed rock masses,Shatuozi pluton is 159~151 Ma,Shicheng Pluton 169~151 Ma,Changyuan Pluton 156~151 Ma,Yunmengshan batholith 146~141 Ma,Fengjiayu—Xibailianyu granite pluton 130~124 Ma,Fengjiayu diorite pluton 127 Ma,Dadonggou granite pluton 127 Ma.Combined with the resultsdating,the cooling rates are calculated.During the development of Sihetang shear zone,the cooling rate of the western,northern and eastern part of the YMCC is 76.92℃/Ma,50.2℃/Ma and 13.7℃/Ma separately.During the development of Dashuiyu shear zone,they are 18.31℃/Ma,6.13℃/Ma and 28.57℃/Ma separately.At the late of the development of YMCC,it is 50.0℃/Ma.Conclusions:The time of Mesozoic magmatic activities and tectonic movements in Yunmenshan area,and the cooling rate around the Yunmengshan batholith in different tectonic evolution stages are worked out.We figure out that there are three stages of magmatic activities:Late Triassic,Late Jurassic and Early Cretaceous.Besides,the Yunmengshan Area suffers three time significant tectonic events.In Early Jurassic,it behaves as the regional angular unconformity in the Yunmengshan area.There are less magmatic activities with the compress movements.In the earlier of Early Cretaceous(143~135.5 Ma),the Sihetang shear zone develops along the northern margin of the Yuanmengshan batholith.In the later of Early Cretaceous,(135~93.9 Ma),the Yunmengshan metamorphic core complex with the Dashuiyu shear zone as the detachment shear zone,develops along the southeastern margin.The northern and western margins of the Yuanmengshan batholith are affected by the Sihetang shear zone and have the higher cooling rate.At the early stage,the eastern margin is less affected by the Sihetang shear zone,with the smaller cooling rate,and mainly behaves the slow isostatic uplift.While at the late stage,with the high influence of the Dashuiyu shear zone,it is of the quick uplift.As a result,in Mesozoic,the Yunmengshan area has suffered many stages magmatic activities and tectonic movements,and it has the different cooling rates in different areas.
Objectives:Mount Yunmeng Area,Beijing locates in the middle part of Yanshan Orogeny,the northern margin of the North China Craton(NCC).In this area,there are many Mesozoic magmatic activities,the E—W-trending thrust Sihetang shear zone,and NE-trending extensional Dashuiyu shear zone.Although,many isotopic dating works have been done for these plutons and movements,there are less works to organize these data to describe their period relationship systematically and discuss their indication to the evolution of the Yunmengshan Metamorphic Core Complex(YMCC)and NCC.Methods:The zircon isotopic dating and single mineral(hornblende and biotite)~(40)Ar/~(39)Ar dating are analyzed in this work.The cooling rates around the Mount Yunmeng are calculated and discussed.Results:Through the Zircon U-Pb isotopic dating,the ages of plutons are defined.The 206 Ma comes from the trapped magma zircon.Among the exposed rock masses,Shatuozi pluton is 159~151 Ma,Shicheng Pluton 169~151 Ma,Changyuan Pluton 156~151 Ma,Yunmengshan batholith 146~141 Ma,Fengjiayu—Xibailianyu granite pluton 130~124 Ma,Fengjiayu diorite pluton 127 Ma,Dadonggou granite pluton 127 Ma.Combined with the resultsdating,the cooling rates are calculated.During the development of Sihetang shear zone,the cooling rate of the western,northern and eastern part of the YMCC is 76.92℃/Ma,50.2℃/Ma and 13.7℃/Ma separately.During the development of Dashuiyu shear zone,they are 18.31℃/Ma,6.13℃/Ma and 28.57℃/Ma separately.At the late of the development of YMCC,it is 50.0℃/Ma.Conclusions:The time of Mesozoic magmatic activities and tectonic movements in Yunmenshan area,and the cooling rate around the Yunmengshan batholith in different tectonic evolution stages are worked out.We figure out that there are three stages of magmatic activities:Late Triassic,Late Jurassic and Early Cretaceous.Besides,the Yunmengshan Area suffers three time significant tectonic events.In Early Jurassic,it behaves as the regional angular unconformity in the Yunmengshan area.There are less magmatic activities with the compress movements.In the earlier of Early Cretaceous(143~135.5 Ma),the Sihetang shear zone develops along the northern margin of the Yuanmengshan batholith.In the later of Early Cretaceous,(135~93.9 Ma),the Yunmengshan metamorphic core complex with the Dashuiyu shear zone as the detachment shear zone,develops along the southeastern margin.The northern and western margins of the Yuanmengshan batholith are affected by the Sihetang shear zone and have the higher cooling rate.At the early stage,the eastern margin is less affected by the Sihetang shear zone,with the smaller cooling rate,and mainly behaves the slow isostatic uplift.While at the late stage,with the high influence of the Dashuiyu shear zone,it is of the quick uplift.As a result,in Mesozoic,the Yunmengshan area has suffered many stages magmatic activities and tectonic movements,and it has the different cooling rates in different areas.
引文
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