黑龙江省东部新元古代—早侏罗世的洋-陆转换过程
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摘要
针对东北微地块群拼贴位置及构造演化这一重要科学问题,运用洋-陆转换及大陆动力学等理论,结合最新研究成果,通过系统分析松嫩地块与佳木斯地块间晚二叠世—晚三叠世嘉荫-牡丹江俯冲增生杂岩(黑龙江杂岩)带的物质组成,甄别了俯冲增生杂岩带内蛇绿岩的类型。研究表明:晚二叠世—晚三叠世蛇绿岩类型主要包括SSZ型蛇绿岩-斜长角闪片岩,地幔柱型蛇绿岩-蓝片岩,洋中脊型蛇绿岩-蓝片岩、超镁铁质岩,与弧盆系演化相关的蛇绿岩超镁铁质岩、辉长岩组合;结合晚二叠世—晚三叠世嘉荫-牡丹江俯冲增生杂岩带和张广才岭杂岩物质组成和各期岩浆弧、区域磨拉石建造空间分布,总结了松嫩地块和佳木斯地块之间新元古代—早侏罗世洋-陆转换过程。
This paper is concerned with an important scientific issue which underlies collage location and tectonic evolution of micro-block groups in Northeast China. The targeted study offers the systematic analysis of material composition of the Jiayin-Mudanjiang subduction accretion complex( Heilongjiang complex) zone between the Songnen and Jiamusi blocks in the Late Permian-Late Triassic by applying the theories such as ocean-land conversion and continental dynamics,and combined with the latest research results; and the subsequent identification of the types of ophiolites in the subduction accretion complex zone. The results show that Late Permian-Late Triassic Ophiolite Types consist mainly of SSZ-type ophiolite-amphibolite schist; mantle plume ophiolite-blueschist; mid-ocean ridge ophiolite-blueschist and ultramafic rock,ophiolite-ultramafic rock and gabbro assemblages related to the evolution of arc basin system;and the combination of the material composition of the Jiayin-Mudanjiang subduction accretion complex belt and the Zhangguangcailing complex and the spatial distribution of magmatic arcs and regional molasses formations in different stages provides a new insight into the Neoproterozoic-Early Jurassic oceaniccontinental transition between Songnen and Jiamusi blocks.
This paper is concerned with an important scientific issue which underlies collage location and tectonic evolution of micro-block groups in Northeast China. The targeted study offers the systematic analysis of material composition of the Jiayin-Mudanjiang subduction accretion complex( Heilongjiang complex) zone between the Songnen and Jiamusi blocks in the Late Permian-Late Triassic by applying the theories such as ocean-land conversion and continental dynamics,and combined with the latest research results; and the subsequent identification of the types of ophiolites in the subduction accretion complex zone. The results show that Late Permian-Late Triassic Ophiolite Types consist mainly of SSZ-type ophiolite-amphibolite schist; mantle plume ophiolite-blueschist; mid-ocean ridge ophiolite-blueschist and ultramafic rock,ophiolite-ultramafic rock and gabbro assemblages related to the evolution of arc basin system;and the combination of the material composition of the Jiayin-Mudanjiang subduction accretion complex belt and the Zhangguangcailing complex and the spatial distribution of magmatic arcs and regional molasses formations in different stages provides a new insight into the Neoproterozoic-Early Jurassic oceaniccontinental transition between Songnen and Jiamusi blocks.
引文
[1] Tang K D. Tectonic development of Paleozoic fold belts at thenorth margin of the Sino-Korean craton[J]. Tectonics,1990,9:249-260.
[2] Liu Y J,Li W M,Feng Z Q,et al. A review of the Paleozoic tec-tonics in the eastern part of Central Asian Orogenic Belt[J].Gondwana Research,2017,43:123-148.
[3]曹熹,党增欣,张兴洲,等.佳木斯复合地体[M].长春:吉林科学技术出版社,1992,45-126.
[4]刘静兰.佳木斯中间地块前寒武纪地质研究[J].长春地质学院学报,1988,18(2):147-156.
[5]周建波,韩杰,张兴洲,等.牡丹江地区蓝片岩的地球化学特征及其大地构造意义[J].吉林大学学报(地球科学版),2010,40(1):93-103.
[6]叶慧文,张兴洲,周欲文.从蓝片岩及蛇绿岩特点看满洲里—绥芬河断面岩石圈结构与演化[M].北京:地震出版社,1994.
[7]李旭平,孔凡梅,郑庆道,等.黑龙江萝北地区黑龙江杂岩年代学研究.岩石学报,2010,26(7):2015-2024.
[8]颉颃强,张福勤,苗来成,等.东北牡丹江地区“黑龙江群”中斜长角闪岩与花岗岩的锆石SHRIMP U-Pb及其地质意义[J].岩石学报,2008,24(6):1237-1250.
[9]吕长禄,肖庆辉,冯俊岭,等.黑龙江依兰地区变玄武岩及变堆晶辉长岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2016,35(7):1081-1094.
[10]吕长禄,冯俊岭,李新鹏,等.依兰地区黑龙江增生杂岩中变质硅质岩的地球化学特征及大地构造背景[J].中国矿业,2016,25(S1):337-341.
[11]周建波,张兴洲,Wilde S A,等.黑龙江杂岩的碎屑锆石年代学及其大地构造意义[J].岩石学报,2009,25(8):1924-1936.
[12]李旭平,焦丽香,郑庆道,等.黑龙江桦南地区黑龙江杂岩锆石U-Pb定年[J].岩石学报,2009,25(8):1909-1916.
[13]赵亮亮.黑龙江杂岩构造演化的岩石学与年代学证据[D].长春:吉林大学,2011.
[14]黑龙江省地质矿产局.黑龙江省区域地质志[M].北京:地质出版社,1993.
[15]付长垒,闫臻,王宗起,等.南祁连拉脊山口增生楔的结构与组成特征[J].岩石学报,2018,34(7):2049-2064.
[16] Wu F Y,Sun D Y,Ge W C,et al. Geochronology of the Phan-erozoic granitoids in northeastern China[J]. Journal of AsianEarth Sciences,2011,41:17-30.
[17]王枫.松嫩—张广才岭地块东缘“元古界”的岩石组合与形成时代:对区域构造演化的意义[D].长春:吉林大学,2013.
[18]张兴洲,乔德武,迟效国,等.东北地区晚古生代构造演化及其石油地质意义[J].地质通报,2011,30(S1):205-213.
[19]谢鸣谦.拼贴板块构造及其驱动机理:中国东北及邻区的大地构造演化[M].北京:科学出版社,2000.
[20]许文良,王枫,裴福萍,等.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J].岩石学报,2013,29(2):339-353.
[21]李锦轶.中国东北及邻区若干地质构造问题的新认识[J].地质论评,1998,44(4):339–347.
[22]刘永江,张兴洲,金巍,等.东北地区晚古生代区域构造演化[J].中国地质,2010,37(4):943-951.
[23]周建波,张兴洲,Simon A W,等.中国东北~500 Ma泛非期孔兹岩带的确定及其意义[J].岩石学报,2011,27(4):1235-1245.
[2] Liu Y J,Li W M,Feng Z Q,et al. A review of the Paleozoic tec-tonics in the eastern part of Central Asian Orogenic Belt[J].Gondwana Research,2017,43:123-148.
[3]曹熹,党增欣,张兴洲,等.佳木斯复合地体[M].长春:吉林科学技术出版社,1992,45-126.
[4]刘静兰.佳木斯中间地块前寒武纪地质研究[J].长春地质学院学报,1988,18(2):147-156.
[5]周建波,韩杰,张兴洲,等.牡丹江地区蓝片岩的地球化学特征及其大地构造意义[J].吉林大学学报(地球科学版),2010,40(1):93-103.
[6]叶慧文,张兴洲,周欲文.从蓝片岩及蛇绿岩特点看满洲里—绥芬河断面岩石圈结构与演化[M].北京:地震出版社,1994.
[7]李旭平,孔凡梅,郑庆道,等.黑龙江萝北地区黑龙江杂岩年代学研究.岩石学报,2010,26(7):2015-2024.
[8]颉颃强,张福勤,苗来成,等.东北牡丹江地区“黑龙江群”中斜长角闪岩与花岗岩的锆石SHRIMP U-Pb及其地质意义[J].岩石学报,2008,24(6):1237-1250.
[9]吕长禄,肖庆辉,冯俊岭,等.黑龙江依兰地区变玄武岩及变堆晶辉长岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2016,35(7):1081-1094.
[10]吕长禄,冯俊岭,李新鹏,等.依兰地区黑龙江增生杂岩中变质硅质岩的地球化学特征及大地构造背景[J].中国矿业,2016,25(S1):337-341.
[11]周建波,张兴洲,Wilde S A,等.黑龙江杂岩的碎屑锆石年代学及其大地构造意义[J].岩石学报,2009,25(8):1924-1936.
[12]李旭平,焦丽香,郑庆道,等.黑龙江桦南地区黑龙江杂岩锆石U-Pb定年[J].岩石学报,2009,25(8):1909-1916.
[13]赵亮亮.黑龙江杂岩构造演化的岩石学与年代学证据[D].长春:吉林大学,2011.
[14]黑龙江省地质矿产局.黑龙江省区域地质志[M].北京:地质出版社,1993.
[15]付长垒,闫臻,王宗起,等.南祁连拉脊山口增生楔的结构与组成特征[J].岩石学报,2018,34(7):2049-2064.
[16] Wu F Y,Sun D Y,Ge W C,et al. Geochronology of the Phan-erozoic granitoids in northeastern China[J]. Journal of AsianEarth Sciences,2011,41:17-30.
[17]王枫.松嫩—张广才岭地块东缘“元古界”的岩石组合与形成时代:对区域构造演化的意义[D].长春:吉林大学,2013.
[18]张兴洲,乔德武,迟效国,等.东北地区晚古生代构造演化及其石油地质意义[J].地质通报,2011,30(S1):205-213.
[19]谢鸣谦.拼贴板块构造及其驱动机理:中国东北及邻区的大地构造演化[M].北京:科学出版社,2000.
[20]许文良,王枫,裴福萍,等.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J].岩石学报,2013,29(2):339-353.
[21]李锦轶.中国东北及邻区若干地质构造问题的新认识[J].地质论评,1998,44(4):339–347.
[22]刘永江,张兴洲,金巍,等.东北地区晚古生代区域构造演化[J].中国地质,2010,37(4):943-951.
[23]周建波,张兴洲,Simon A W,等.中国东北~500 Ma泛非期孔兹岩带的确定及其意义[J].岩石学报,2011,27(4):1235-1245.
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