The timing of the initial Indo-Asian collision is a subject of debate for a long time.Besides,the magmatic trace of the collisional process is also unclear.In the present study,the authors report Early Eocene leucocra...The timing of the initial Indo-Asian collision is a subject of debate for a long time.Besides,the magmatic trace of the collisional process is also unclear.In the present study,the authors report Early Eocene leucocratic sill/dike swarms in the northern edge of the Nymo intrusive complex of the Gangdese belt,southern Tibet.The Nymo intrusive complex was emplaced at ca.50–47 Ma and surrounded by the metamorphosed Jurassic-aged Bima Formation volcano-sedimentary sequence along its northern side.At outcrops,the leucocratic sills/dikes intruded along or truncated the deformed foliations of the host Bima Formation,which has been subject to high-temperature amphibolite-facies metamorphism at ca.50–47 Ma.Detailed cathodoluminescence image analyses reveal that the zircon grains of the leucocratic sills/dikes have core-mantle textures.The cores yield the Jurassic ages comparable to the protolith ages of the Bima Formation.In contrast,the mantles of zircon grains yield weighted mean ages of ca.49–47 Ma,representing the crystallization timing of these leucocratic sills/dikes.The coeval ages for the Nymo intrusive complex,the high-temperature metamorphism,and the leucocratic sills/dikes indicate that a close relationship exists among them.The authors tentatively suggest that these leucocratic sills/dikes were generated from partial melting of the Jurassic-aged Bima Formation volcanic rocks,triggered by the high heat from the magma chamber of the Nymo intrusive complex.This Early Eocene tectono-thermal event of coeval magmatism,metamorphism and partial melting was most likely formed during the Indo-Asian collisional setting.展开更多
北衙金多金属矿田是藏东-金沙江-哀牢山新生代富碱斑岩成矿带中南段的代表性矿床之一,发育一个与富碱斑岩密切相关的金多金属成矿系统。本文较为系统地分析了矿田内的成岩成矿作用特征及其演化过程,并探讨其与印-亚碰撞造山过程的响应...北衙金多金属矿田是藏东-金沙江-哀牢山新生代富碱斑岩成矿带中南段的代表性矿床之一,发育一个与富碱斑岩密切相关的金多金属成矿系统。本文较为系统地分析了矿田内的成岩成矿作用特征及其演化过程,并探讨其与印-亚碰撞造山过程的响应关系。富碱斑岩具有埃达克岩的地球化学亲合性,其源区是喜马拉雅期印-亚碰撞造山造成的软流圈向东挤出汇聚使大规模走滑断裂活化,诱发玄武质下地壳部分熔融的壳幔过渡层,成岩年龄可分为第一期(65～59Ma)、第二期(36～32Ma)、第三期(26～24Ma)和最晚期(3.8～3.6Ma)等4期,其中第二、三期与富碱岩带北段的两期岩浆集中活动时期基本吻合,形成的斑岩对金多金属成矿较为有利。区内金多金属矿床可划分为三个矿床类型和七个矿床亚类,即与喜马拉雅早—中期斑岩有关的金多金属矿床(Ⅰ),包括接触带夕卡岩型、斑岩型和热液充填型(及熔浆型)金多金属矿床;与喜马拉雅第三期斑岩有关的金多金属矿床(Ⅱ),包括爆破角砾岩型和叠加热液改造型金多金属矿床;以及与喜马拉雅期表生作用有关的风化堆积型金矿床(Ⅲ),包括古砂矿型和红色粘土型金矿床。Ⅰ、Ⅱ类型矿床受富碱斑岩及伴生的 NE 到 NNE 向断裂控制,赋存于富碱斑岩体内、内外接触带及其附近围岩的层间破碎带或构造裂隙带中,在成因和空间上与斑岩及隐爆角砾岩等密切有关。成矿物质和成矿流体主要来源于地幔,围岩地层只是提供了成矿的空间,不同类型的矿体之间呈"贯通式"的时间和空间关系,构成了一个统一的喜马拉雅期富碱斑岩-热液型金多金属成矿系统。先期形成矿床明显受后期岩浆热液的叠加改造,但矿化分布和成矿元素组合仍表现为以斑岩为中心,存在 CuAu(Mo)多金属→FeCuAuPbZn 多金属→AuPhZnAg 多金属的分带特征。从最早期含金铁矿床形成之后,原生金矿的次生富集和表生成矿作用就已开始,并形成不同成因类型的风化-堆积型金矿床。其中,古红色粘土型金矿床的成矿主要发生在始新世到渐新世,河-湖相古砂金矿床形成于23～5Ma 期间,红色粘土型(残坡积型)金矿床可从始新世一直延续至今。通过与区域斑岩成岩成矿演化时序的对比,提出与藏东-金沙江-哀牢山斑岩成矿带上的众多矿床一样,北衙矿田内的成岩成矿作也是喜马拉雅期印-亚陆陆碰撞造山带成岩成矿作用在东南缘构造转换带的远程效应,记录了印-亚大陆碰撞造山的详细过程。因而,该矿田深部及外围地区,仍存在巨大的找矿潜力。盐源-丽江断裂带可能也是一务与藏东-金沙江.哀牢山斑岩成矿带联系密切而又相对独立的富碱斑岩成矿带。展开更多
The Eurasian continent was subject to multiphase intensive intracontinental deformation in the Cenozoic(Fig.1A).However,its Cenozoic intra-continental deformation process and the driving force has long been disputed,w...The Eurasian continent was subject to multiphase intensive intracontinental deformation in the Cenozoic(Fig.1A).However,its Cenozoic intra-continental deformation process and the driving force has long been disputed,which is only associated with the Indo-Asian collision(Molnar and Tapponnier,1975;Jolivet et al.,1990;Tapponnier et al.,2001;Yin,2010;Xu et al.,2013;Zhao et al.,2016),is caused by the Pacific-Asian collision(Cui,1997;Schellart and Lister,2005;Fan et al.,2019),or is connected with a combined effect of the Indo-Asian collision and the Pacific-Eurasia convergence(Ren et al.,2002;Li et al.,2013;Shi et al.,2015;Liu et al.,2019).展开更多
基金the National Key Research and Development Project“Key scientific issues of transformative technology”(2019YFA0708601)the Key Special Project for Introduced Talents Team of the Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou)(GML2019ZD0201)+4 种基金the second Tibetan Plateau Scientific Expedition and Research Program(STEP)Grant(2019QZKK0802)the Research Grants of Chinese Academy of Geological Sciences(J2024)the Geological Survey of China(DD20190057 and DD20190060)the National Natural Science Foundation of China(41502198)the open fund of State Key Laboratory for Mineral Deposits Research at Nanjing University(2020-LAMD-K04).
文摘The timing of the initial Indo-Asian collision is a subject of debate for a long time.Besides,the magmatic trace of the collisional process is also unclear.In the present study,the authors report Early Eocene leucocratic sill/dike swarms in the northern edge of the Nymo intrusive complex of the Gangdese belt,southern Tibet.The Nymo intrusive complex was emplaced at ca.50–47 Ma and surrounded by the metamorphosed Jurassic-aged Bima Formation volcano-sedimentary sequence along its northern side.At outcrops,the leucocratic sills/dikes intruded along or truncated the deformed foliations of the host Bima Formation,which has been subject to high-temperature amphibolite-facies metamorphism at ca.50–47 Ma.Detailed cathodoluminescence image analyses reveal that the zircon grains of the leucocratic sills/dikes have core-mantle textures.The cores yield the Jurassic ages comparable to the protolith ages of the Bima Formation.In contrast,the mantles of zircon grains yield weighted mean ages of ca.49–47 Ma,representing the crystallization timing of these leucocratic sills/dikes.The coeval ages for the Nymo intrusive complex,the high-temperature metamorphism,and the leucocratic sills/dikes indicate that a close relationship exists among them.The authors tentatively suggest that these leucocratic sills/dikes were generated from partial melting of the Jurassic-aged Bima Formation volcanic rocks,triggered by the high heat from the magma chamber of the Nymo intrusive complex.This Early Eocene tectono-thermal event of coeval magmatism,metamorphism and partial melting was most likely formed during the Indo-Asian collisional setting.
文摘北衙金多金属矿田是藏东-金沙江-哀牢山新生代富碱斑岩成矿带中南段的代表性矿床之一,发育一个与富碱斑岩密切相关的金多金属成矿系统。本文较为系统地分析了矿田内的成岩成矿作用特征及其演化过程,并探讨其与印-亚碰撞造山过程的响应关系。富碱斑岩具有埃达克岩的地球化学亲合性,其源区是喜马拉雅期印-亚碰撞造山造成的软流圈向东挤出汇聚使大规模走滑断裂活化,诱发玄武质下地壳部分熔融的壳幔过渡层,成岩年龄可分为第一期(65～59Ma)、第二期(36～32Ma)、第三期(26～24Ma)和最晚期(3.8～3.6Ma)等4期,其中第二、三期与富碱岩带北段的两期岩浆集中活动时期基本吻合,形成的斑岩对金多金属成矿较为有利。区内金多金属矿床可划分为三个矿床类型和七个矿床亚类,即与喜马拉雅早—中期斑岩有关的金多金属矿床(Ⅰ),包括接触带夕卡岩型、斑岩型和热液充填型(及熔浆型)金多金属矿床;与喜马拉雅第三期斑岩有关的金多金属矿床(Ⅱ),包括爆破角砾岩型和叠加热液改造型金多金属矿床;以及与喜马拉雅期表生作用有关的风化堆积型金矿床(Ⅲ),包括古砂矿型和红色粘土型金矿床。Ⅰ、Ⅱ类型矿床受富碱斑岩及伴生的 NE 到 NNE 向断裂控制,赋存于富碱斑岩体内、内外接触带及其附近围岩的层间破碎带或构造裂隙带中,在成因和空间上与斑岩及隐爆角砾岩等密切有关。成矿物质和成矿流体主要来源于地幔,围岩地层只是提供了成矿的空间,不同类型的矿体之间呈"贯通式"的时间和空间关系,构成了一个统一的喜马拉雅期富碱斑岩-热液型金多金属成矿系统。先期形成矿床明显受后期岩浆热液的叠加改造,但矿化分布和成矿元素组合仍表现为以斑岩为中心,存在 CuAu(Mo)多金属→FeCuAuPbZn 多金属→AuPhZnAg 多金属的分带特征。从最早期含金铁矿床形成之后,原生金矿的次生富集和表生成矿作用就已开始,并形成不同成因类型的风化-堆积型金矿床。其中,古红色粘土型金矿床的成矿主要发生在始新世到渐新世,河-湖相古砂金矿床形成于23～5Ma 期间,红色粘土型(残坡积型)金矿床可从始新世一直延续至今。通过与区域斑岩成岩成矿演化时序的对比,提出与藏东-金沙江-哀牢山斑岩成矿带上的众多矿床一样,北衙矿田内的成岩成矿作也是喜马拉雅期印-亚陆陆碰撞造山带成岩成矿作用在东南缘构造转换带的远程效应,记录了印-亚大陆碰撞造山的详细过程。因而,该矿田深部及外围地区,仍存在巨大的找矿潜力。盐源-丽江断裂带可能也是一务与藏东-金沙江.哀牢山斑岩成矿带联系密切而又相对独立的富碱斑岩成矿带。
基金supported by the National Natural Science Foundation of China(Grant No.41672203)China Geological Survey(CGS)(Grant Nos.DD20190018,DD20160060,1212011120099,1212011120100,1212011220259).
文摘The Eurasian continent was subject to multiphase intensive intracontinental deformation in the Cenozoic(Fig.1A).However,its Cenozoic intra-continental deformation process and the driving force has long been disputed,which is only associated with the Indo-Asian collision(Molnar and Tapponnier,1975;Jolivet et al.,1990;Tapponnier et al.,2001;Yin,2010;Xu et al.,2013;Zhao et al.,2016),is caused by the Pacific-Asian collision(Cui,1997;Schellart and Lister,2005;Fan et al.,2019),or is connected with a combined effect of the Indo-Asian collision and the Pacific-Eurasia convergence(Ren et al.,2002;Li et al.,2013;Shi et al.,2015;Liu et al.,2019).
