必须声明标量变量 "@Script_ID"。 南秦岭构造带十堰—武当地区岩石变质作用-《地球科学与环境学报》
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[1]王东升,王宗起*,王刚,等.南秦岭构造带十堰—武当地区岩石变质作用[J].地球科学与环境学报,2019,41(04):379-395.
 WANG Dong-sheng,WANG Zong-qi*,WANG Gang,et al.Metamorphism of Rocks in Shiyan-Wudang Area of South Qinling Tectonic Belt, China[J].Journal of Earth Sciences and Environment,2019,41(04):379-395.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第04期
页码:
379-395
栏目:
基础地质与矿产地质
出版日期:
2019-07-15

文章信息/Info

Title:
Metamorphism of Rocks in Shiyan-Wudang Area of South Qinling Tectonic Belt, China
文章编号:
1672-6561(2019)04-0379-17
作者:
王东升王宗起*王刚武昱东杨皓
(中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室,北京 100037)
Author(s):
WANG Dong-sheng WANG Zong-qi* WANG Gang WU Yu-dong YANG Hao
(MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China)
关键词:
变质作用 印支期 片岩 绿片岩相 中低级变质岩 俯冲-增生 十堰—武当地区 南秦岭
Keywords:
metamorphism Indosinian schist greenschist facies middle- and low-grade metamorphic rocks subduction-accretion Shiyan-Wudang area South Qinling
分类号:
P588.34
DOI:
-
文献标志码:
A
摘要:
十堰—武当地区位于南秦岭构造带和扬子板块的结合部位,内部发育的变质岩可为秦岭造山带印支期造山过程提供重要信息。在该地区含石榴子石片岩的岩石学、矿物学研究基础上,利用石榴子石-黑云母地质温度计和石榴子石-白云母地质温度计计算变质作用条件。结果表明:石榴子石-黑云母地质温度计计算得到方滩—王家山剖面南、北两侧变质岩的主期变质温度分别为344 ℃~410 ℃和368 ℃~431 ℃,属于低绿片岩相; 由石榴子石-白云母地质温度计计算得到十堰—大木剖面南、北两侧变质岩主期变质温度分别为322 ℃~440 ℃和535 ℃~540 ℃,属于低—高绿片岩相。结合区域变质变形研究成果,认为十堰—武当地区中低级变质岩的变质作用演化与南秦岭构造带印支期洋盆闭合伴生的俯冲-增生过程有关,它使得不同变质级别的岩石发生并置然后一起抬升。
Abstract:
Shiyan-Wudang area is located at the junction of South Qinling tectonic belt and Yangtze plate. Its metamorphism can provide important information for Indosinian orogenic process of Qinling orogenic belt. Based on the study of petrology and mineralogy of garnet-bearing schist in Shiyan-Wudang area, the metamorphic conditions were calculated by using garnet-biotite geothermometer and garnet-muscovite geothermometer. The results show that main metamorphism temperatures of metamorphic rocks from south and north parts of Fangtan-Wangjiashan section calculated by garnet-biotite geothermometer are 344 ℃-410 ℃ and 368 ℃-431 ℃, which are in agreement with lower greenschist facies; meanwhile, main metamorphism temperatures of metamorphic rocks from south and north parts of Shiyan-Damu section calculated by garnet-muscovite geothermometer are 322 ℃-440 ℃ and 535 ℃-540 ℃, agreeing with lower to higher greenschist facies condition. Combining with regional metamorphism and deformation data, it is suggested that metamorphic evolution of middle- and low-grade metamorphic rocks in Shiyan-Wudang area is related to the subduction-accretion process caused by the closure of ocean in South Qinling tectonic belt during Indosinian, which juxtaposes different grades of metamorphic rocks and makes them uplift together.

参考文献/References:

[1] 吉成林,李明荣,王仁民.恒山东段新太古杂岩两种 P-T-t 轨迹的确定及其意义[J].岩石矿物学杂志,1993,12(1):32-39.
JI Cheng-lin,LI Ming-rong,WANG Ren-min.Determination and Significance of Two P-T-t Paths in the Neoarchean Complex of Eastern Hengshan[J].Acta Petrologica et Mineralogica,1993,12(1):32-39.
[2] ST-ONGE M R.Zoned Poikiloblastic Garnets:P-T Paths and Syn-metamorphic Uplift Through 30 km of Structural Depth,Wopmay Orogen,Canada[J].Journal of Petrology,1987,28(1):1-21.
[3] ZHANG R Y,LIOU J G.Coesite-bearing Eclogite in Henan Province,Central China:Detailed Petrography,Glaucophane Stability and P-T Path[J].European Journal of Mineralogy,1994,6(2):217-233.
[4] 游振东.变质地质学的三大前缘课题[J].地学前缘,1994,1(1/2):111-124.
YOU Zhen-dong.Review of Metamorphic Geology and Its Prospects[J].Earth Science Frontiers,1994,1(1/2):111-124.
[5] 魏春景.变质作用 P-T-t 轨迹的研究方法与进展[J].地学前缘,2011,18(2):1-16.
WEI Chun-jing.Approaches and Advancement of the Metamorphic P-T-t Paths[J].Earth Science Frontiers,2011,18(2):1-16.
[6] 卢良兆.变质作用 P-T-t 轨迹及其地球动力学意义[J].国外前寒武纪地质,1991(3):4-20.
LU Liang-zhao.Metamorphic P-T-t Paths and Its Geo-dynamic Significance[J].Overseas Precambrian Cambrian Geology,1991(3):4-20.
[7] LIOU J G,ERNST W G,ZHANG R Y,et al.Ultrahigh-pressure Minerals and Metamorphic Terranes:The View from China[J].Journal of Asian Earth Sciences,2009,35(3/4):199-231.
[8] 张忠义,吴淦国,宋明春,等.苏鲁高压—超高压带的结构、变形特征及形成背景探讨[J].地球学报,2004,25(6):607-614.
ZHANG Zhong-yi,WU Gan-guo,SONG Ming-chun,et al.Texture,Deformation and Formation Background of the Sulu High-ultrahigh Pressure Metamorphic Belt[J].Acta Geoscientica Sinica,2004,25(6):607-614.
[9] 王清晨.中国超高压变质岩十五年研究进展[J].地球学报,2001,22(1):11-16.
WANG Qing-chen.Development of Studying Ultrahigh-pressure Metamorphic Rocks from China During the Past 15 Years[J].Acta Geoscientica Sinica,2001,22(1):11-16.
[10] 张泽明,沈 昆.大陆俯冲带的深部流体及变质化学地球动力学:以苏鲁超高压变质带为例[J].地球学报,2009,30(1):5-20.
ZHANG Ze-ming,SHEN Kun.Fluids from the Deeply Continental Subduction Zone and the Metamorphic Chemical Geodynamics[J].Acta Geoscientica Sinica,2009,30(1):5-20.
[11] 李 才,董永胜,翟庆国,等.青藏高原羌塘高压变质带的特征及其构造意义[J].地质通报,2008,27(1):27-35.
LI Cai,DONG Yong-sheng,ZHAI Qing-guo,et al.High-pressure Metamorphic Belt in Qiangtang,Qinghai-Tibet Plateau,and Its Tectonic Significance[J].Geological Bulletin of China,2008,27(1):27-35.
[12] 许志琴,张泽明,刘福来,等.苏鲁高压—超高压变质带的折返构造及折返机制[J].地质学报,2003,77(4):433-450.
XU Zhi-qin,ZHANG Ze-ming,LIU Fu-lai,et al.Exhumation Structure and Mechanism of the Sulu Ultrahigh-pressure Metamorphic Belt,Central China[J].Acta Geologica Sinica,2003,77(4):433-450.
[13] 游振东.超高压变质带的全球分布及其大地构造意义[J].高校地质学报,2007,13(3):383-391.
YOU Zhen-dong.Global Distribution of Ultrahigh-pressure Metamorphic Belts and Its Geotectonic Significance[J].Geological Journal of China Universities,2007,13(3):383-391.
[14] 郑永飞.超高压变质与大陆碰撞研究进展:以大别—苏鲁造山带为例[J].科学通报,2008,53(18):2129-2152.
ZHENG Yong-fei.A Perspective View on Ultrahigh-pressure Metamorphism and Continental Collision in the Dabie-Sulu Orogenic Belt[J].Chinese Science Bulletin,2008,53(18):2129-2152.
[15] 刘 良,曹玉亭,陈丹玲,等.南阿尔金与北秦岭高压—超高压变质作用研究新进展[J].科学通报,2013,58(22):2113-2123.
LIU Liang,CAO Yu-ting,CHEN Dan-ling,et al.New Progresses on the HP-UHP Metamorphism in the South Altyn Tagh and the North Qinling[J].Chinese Science Bulletin,2013,58(22):2113-2123.
[16] 宋述光,张贵宾,张 聪,等.大洋俯冲和大陆碰撞的动力学过程:北祁连—柴北缘高压—超高压变质带的岩石学制约[J].科学通报,2013,58(23):2240-2245.
SONG Shu-guang,ZHANG Gui-bin,ZHANG Cong,et al.The Dynamics of Oceanic Subduction and Continental Collision:The Petrological Constraints of HP-UHP Metamorphic Belt in North Qilian-North Qai-dam[J].Chinese Science Bulletin,2013,58(23):2240-2245.
[17] 张建新,杨经绥,许志琴,等.阿尔金榴辉岩中超高压变质作用证据[J].科学通报,2002,47(3):231-234.
ZHANG Jian-xin,YANG Jing-sui,XU Zhi-qin,et al.Evidence for UHP Metamorphism of Eclogites from the Altun Mountains[J].Chinese Science Bulletin,2002,47(3):231-234.
[18] 钟大赉,丁 林.西藏南迦巴瓦峰地区发现高压麻粒岩[J].科学通报,1995,40(14):1343.
ZHONG Da-lai,DING Lin.Discovery of High-pressure Basic Granulite in Namjiagbarwa Area,Tibet,China[J].Chinese Science Bulletin,1995,40(14):1343.
[19] 刘 良,廖小莹,张成立,等.北秦岭高压—超高压岩石的多期变质时代及其地质意义[J].岩石学报,2013,29(5):1634-1656.
LIU Liang,LIAO Xiao-ying,ZHANG Cheng-li,et al.Multi-metamorphic Timings of HP-UHP Rocks in the North Qinling and Their Geological Implications[J].Acta Petrologica Sinica,2013,29(5):1634-1656.
[20] 刘福来,薛怀民.苏鲁—大别超高压岩石中锆石SHRI-
MP U-Pb定年研究:综述和最新进展[J].岩石学报,2007,23(11):2737-2756.
LIU Fu-lai,XUE Huai-min.Review and Prospect of SHRIMP U-Pb Dating on Zircons from Sulu-Dabie UHP Metamorphic Rocks[J].Acta Petrologica Sinica,2007,23(11):2737-2756.
[21] 蔡学林,石绍清,吴德超,等.武当山推覆体构造的形成与演化[M].成都:成都科技大学出版社,1995.
CAI Xue-lin,SHI Shao-qing,WU De-chao,et al.Formation and Tectonic Evolution of the Wudangshan Nappe Structure[M].Chengdu:Chengdu University of Science and Technology Press,1995.
[22] 方向池,蔡学林,王寿琼.推覆构造的控矿成矿规律:以武当山推覆构造为例[J].成都地质学院学报,1993,20(4):34-37.
FANG Xiang-chi,CAI Xue-lin,WANG Shou-qiong.Regularity Controlling Ore Distribution and Mineralization of Nappe Tectonics[J].Journal of Chengdu College of Geology,1993,20(4):34-37.
[23] 石绍清.武当山推覆体中段的叠加褶皱及构造序列的初步划分[J].成都地质学院学报,1993,20(4):18-26.
SHI Shao-qing.Primary Division of the Superimposed Fold and Tectonic Sequence in the Middle Section of Wudang Mountain Nappes[J].Journal of Chengdu College of Geology,1993,20(4):18-26.
[24] 蔡学林,魏显贵,吴德超,等.武当山推覆构造结构模式[J].成都地质学院学报,1988,15(4):33-42.
CAI Xue-lin,WEI Xian-gui,WU De-chao,et al.Nappe Structure in the Wudang Mountains[J].Journal of Chengdu College of Geology,1988,15(4):33-42.
[25] 石绍清,蔡学林,吴德超,等.武当山推覆构造的几何结构:鳞片叠覆模式[J].成都理工学院学报,1995,22(4):46-53.
SHI Shao-qing,CAI Xue-lin,WU De-chao,et al.Geometric Structure of the Nappe Tectonic of Wudang Mountain:A Scaly Imbrication Model[J].Journal of Chengdu Institute of Technology,1995,22(4):46-53.
[26] 徐贵忠,王艺芬,张稳胜.桐柏—大别山碰撞造山带的大地构造演化[J].西安地质学院学报,1993,15(1):35-44.
XU Gui-zhong,WANG Yi-fen,ZHANG Wen-sheng.The Geological Evolution of the Collision Type Orogenic Belt in the Tongbai-Dabieshan Mountain[J].Journal of Xi’an College of Geology,1993,15(1):35-44.
[27] 秦正永,陈林栋,刘兴义,等.武当地区构造类型及其控矿作用[J].地质调查与研究,2005,28(1):16-24.
QIN Zheng-yong,CHEN Lin-dong,LIU Xing-yi,et al.Structural Types and Ore-controlling Process in Wudang Area[J].Geological Survey and Research,2005,28(1):16-24.
[28] 雷世和,唐桂英.南秦岭造山带武当地区构造变形及构造复合[J].河北地质学院学报,1996,19(3/4):278-284.
LEI Shi-he,TANG Gui-ying.Study on Structural Deformation and Tectonic Compound in Wudang Area,Southern Qinling Orogen[J].Journal of Hebei College of Geology,1996,19(3/4):278-284.
[29] 朱章显.武当山岩群杨坪岩组叠加褶皱[J].湖北地矿,1998,12(1):7-12.
ZHU Zhang-xian.Superimposed Folds in Yangping Rock Formation of Wudangshan Rock Group[J].Hubei Geology and Mineral Resources,1998,12(1):7-12.
[30] 刘兴义,陈盛锋,蔡志勇.武当地区构造类型及控矿特征[J].湖北地质,1997,11(2):1-10.
LIU Xing-yi,CHEN Sheng-feng,CAI Zhi-yong.Structural Types and Their Ore-control Characteristics in Wudang Area[J].Hubei Geology,1997,11(2):1-10.
[31] 朱 杰.武当隆起与扬子地块接触带逆冲推覆构造的基本特征[J].湖北地质,1994,8(1):32-38.
ZHU Jie.The Overthrust Nappe Structure in the Contact Zone Between Wudang Uplift and Yangtze Massif[J].Hubei Geology,1994,8(1):32-38.
[32] 张业明,付建明,蔡锦辉,等.武当地区构造格架及其对矿产的控制[J].华南地质与矿产,1999(4):16-20.
ZHANG Ye-ming,FU Jian-ming,CAI Jin-hui,et al.Tectonic Framework and Its Control over Mineralization in Wudang Area[J].Geology and Mineral Resources of South China,1999(4):16-20.
[33] 陈晋镳,秦正永,王寿琼,等.武当群地质特征[M].天津:天津科技翻译出版公司,1991.
CHEN Jin-biao,QIN Zheng-yong,WANG Shou-qiong,et al.The Geological Characteristics of Wudang Group[M].Tianjin:Tianjin Science and Technology Translation and Publishing Company,1991.
[34] 刘庆祥.鄂西北武当群矿物学特征及变质作用研究[J].武汉化工学院学报,1994,16(1):23-29.
LIU Qing-xiang.A Study of Mineral Characteristics and Metamorphism Within Wudang Group in Northwestern Hubei[J].Journal of Wuhan Institute of Chemical Technolgy,1994,16(1):23-29.
[35] 张国伟,孟庆任.秦岭造山带的结构构造[J].中国科学:B 辑,1995,25(9):994-1003.
ZHANG Guo-wei,MENG Qing-ren.Tectonics and Structure of Qinling Orogenic Belt[J].Science in China:Series B,1995,25(9):994-1003.
[36] 张国伟,董云鹏,姚安平.秦岭造山带基本组成与结构及其构造演化[J].陕西地质,1997,15(2):1-14.
ZHANG Guo-wei,DONG Yun-peng,YAO An-ping.The Crustal Compositions,Structures and Tectonic Evolution of the Qinling Orogenic Belt[J].Geology of Shaanxi,1997,15(2):1-14.
[37] 赖绍聪,张国伟,杨永成,等.南秦岭勉县—略阳结合带蛇绿岩与岛弧火山岩地球化学及其大地构造意义[J].地球化学,1998,27(3):283-293.
LAI Shao-cong,ZHANG Guo-wei,YANG Yong-cheng,et al.Geochemistry of the Ophiolite and Island-arc Volcanic Rocks in the Mianxian-Lueyang Suture Zone,Southern Qinling and Their Tectonic Significance[J].Geochimica,1998,27(3):283-293.
[38] LI S Z,KUSKY T M,WANG L,et al.Collision Leading to Multiple-stage Large-scale Extrusion in the Qinling Orogen:Insights from the Mianlue Suture[J].Gondwana Research,2007,12(1/2):121-143.
[39] FAURE M,LIN W,MONIE P,et al.Palaeozoic Collision Between the North and South China Blocks,Triassic Intracontinental Tectonics,and the Problem of the Ultrahigh-pressure Metamorphism[J].Comptes Rendus Geoscience,2008,340(2/3):139-150.
[40] DONG Y P,ZHANG G W,NEUBAUER F,et al.Tectonic Evolution of the Qinling Orogen,China:Review and Synthesis[J].Journal of Asian Earth Sciences,2011,41(3):213-237.
[41] 杨森楠,吴 鉴,杨学忠,等.大别山前寒武纪构造演化[J].地球科学,1983,3(2):81-91.
YANG Sen-nan,WU Jian,YANG Xue-zhong,et al.Precambrian Tectonic Evolution of Dabie Shan[J].Earth Science,1983,3(2):81-91.
[42] 吴利仁,徐贵忠.东秦岭—大别山碰撞造山带的地质演化[M].北京:科学出版社,1998.
WU Li-ren,XU Gui-zhong.Geological Evolution of Eastern Qinling-Dabie Collisional Orogenic Belt[M].Beijing:Science Press,1998.
[43] 徐树桐,刘贻灿,吴维平,等.大别山造山带研究的主要进展及存在问题[J].自然科学进展,2001,11(8):796-803.
XU Shu-tong,LIU Yi-can,WU Wei-ping,et al.The Main Research Progress and the Existing Problems in Dabie Orogenic Belt[J].Progress in Natural Science,2001,11(8):796-803.
[44] 王 荃,刘雪亚.是岩浆侵入还是构造侵位?——湖北两郧—随枣镁铁岩带野外调查纪实[J].地质论评,2010,56(3):329-338.
WANG Quan,LIU Xue-ya.Is Magmatic Intrusion or Exotic Block Emplacement?—Field Survey and Records of Yunxi-Suizhou Mafic Magmatic Belt in Hubei Province[J].Geological Review,2010,56(3):329-338.
[45] 王宗起,武昱东,马昌前.武当—桐柏—大别关键地区区域地质调查成果报告[R].北京:中国地质科学院矿产资源研究所,2016.
WANG Zong-qi,WU Yu-dong,MA Chang-qian.Regional Geological Survey Report of Wudang-Tongbai-Dabie Area[R].Beijing:Institute of Mineral Resources,Chinese Academy of Geological Sciences,2016.
[46] 雷世和,唐桂英,张子才.鄂西北竹山银洞沟银金矿床构造控矿特征[J].现代地质,1998,12(3):374-379.
LEI Shi-he,TANG Gui-ying,ZHANG Zi-cai.Characteristics of Structurally Controlling Mineralization in the Yindonggou Silver-gold Deposit,Zhushan,Northwest Hubei[J].Geoscience,1998,12(3):374-379.
[47] 凌文黎,任邦方,段瑞春,等.南秦岭武当群、耀岭河群及基性侵入岩群锆石U-Pb同位素年代学及其地质意义[J].科学通报,2007,52(12):1445-1456.
LING Wen-li,REN Bang-fang,DUAN Rui-chun,et al.Timing of the Wudangshan,Yaolinghe Volcanic Sequences and Mafic Sills in South Qinling:Zircon U-Pb Geochronology and Tectonic Implication[J].Chinese Science Bulletin,2007,52(12):1445-1456.
[48] 李金发,张业明,罗玉祖.鄂西北许家坡金银矿床地质地球化学特征及成因分析[J].地质科技情报,2003,22(4):75-79.
LI Jin-fa,ZHANG Ye-ming,LUO Yu-zu.Geological-geochemical Characteristics and Genesis Analysis of Xujiapo Gold-silver Deposit in Northwest Hubei Province[J].Geological Science and Technology Information,2003,22(4):75-79.
[49] 付建明,张业明,蔡锦辉.武当—两郧地区主要赋矿地层及其成矿元素[J].地质科技情报,2004,23(2):51-56.
FU Jian-ming,ZHANG Ye-ming,CAI Jin-hui.Cha-racteristics of Main Ore-host Strata and Their Metallogenic Elements in Wudang-Yunxi and Yunxian Region[J].Geological Science and Technology Information,2004,23(2):51-56.
[50] 刘兴义,周骏华.湖北省武当山地区银金矿多金属矿成矿地质条件的分析及找矿方向的初步认识[J].中国区域地质,1985(3):171-180.
LIU Xing-yi,ZHOU Jun-hua.Analysis of the Conditions for Electrum and Polymetallic Deposit Formation in the Wudang Mountains Area,Hubei Province and Preliminary Recognition on the Direction in Mineral Prospecting[J].Regional Geology of China,1985(3):171-180.
[51] 胡健民,赵国春,孟庆任,等.武当地块基性侵入岩群的地质特征与构造意义[J].岩石学报,2003,19(4):601-611.
HU Jian-min,ZHAO Guo-chun,MENG Qing-ren,et al.Basic Sill Swarms in Wudang Block of the Southern Qinling and Its Geological Significance[J].Acta Petrologica Sinica,2003,19(4):601-611.
[52] 林长谦,刘兴义,何洪涛,等.湖北武当地区上震旦—下寒武统黑色岩系含矿性分析[J].资源环境与工程,2006,20(1):1-5.
LIN Chang-qian,LIU Xing-yi,HE Hong-tao,et al.The Ore Potentiality of the Upper Sinian-Lower Cambrian Black Rock Sequence in Wudang Region of Hubei[J].Resources Environment and Engineering,2006,20(1):1-5.
[53] 汪东波,张本仁,马振东.鄂西北地区武当群地球化学及金银含矿性评价[J].地质找矿论丛,1991,6(1):14-27.
WANG Dong-bo,ZHANG Ben-ren,MA Zhen-dong.The Geochemistry and Appraisal of Gold-silver Bearing Ability of Wudangshan Group in Hubei Province[J].Contributions to Geology and Mineral Resources Research,1991,6(1):14-27.
[54] 林长谦,胡 明,何洪涛.湖北武当地区银金多金属矿控矿条件及找矿方向[J].地质找矿论丛,2006,21(2):104-108.
LIN Chang-qian,HU Ming,HE Hong-tao.Ore-control Condition and Ore-searching Direction of Ag-Au Polymetal Deposits in Wudang Area,Hubei Province[J].Contributions to Geology and Mineral Resources Research,2006,21(2):104-108.
[55] 蔡志慧,李化启,唐哲民,等.雪球状石榴子石变斑晶的形成机制:以南迦巴瓦地区雅鲁藏布江缝合带西侧石英片岩为例[J].地学前缘,2010,17(1):61-73.
CAI Zhi-hui,LI Hua-qi,TANG Zhe-min,et al.The Formation Mechanism of Garnet Porphyroblast with Snowball Structure:A Case Study from the Quartz Schist in West Indus-Yarlung Tsangpo Suture Zone,Namche Barwa,Tibet[J].Earth Science Frontiers,2010,17(1):61-73.
[56] 陈能松,孙 敏,杨 勇,等.变质石榴石的成分环带与变质过程[J].地学前缘,2003,10(3):315-320.
CHEN Neng-song,SUN Min,YANG Yong,et al.Major- and Trace-element Zoning in Metamorphic Garnets and Their Metamorphic Process Implications[J].Earth Science Frontiers,2003,10(3):315-320.
[57] MIYASHIRO A,MIYASHIRO A.Metamorphism and
Metamorphic Belts[M].London:Wiley,1973.
[58] 胡恭任.赣中周潭群变质岩中石榴石的演化史及其地质意义[J].矿物岩石,2007,27(2):33-38.
HU Gong-ren.The Chemical Composition,Mineral Evolution and the Significance of Garnet from the Zhoutan Group in Central Jiangxi Province[J].Journal of Mineralogy and Petrology,2007,27(2):33-38.
[59] WU C M,ZHANG J,REN L D.Empirical Garnet-bio-
tite-plagioclase-quartz(GBPQ)Geobarometry in Medium- to High-grade Metapelites[J].Journal of Petro-logy,2004,45(9):1907-1921.
[60] HOLDAWAY M J.Application of New Experimental and Garnet Margules Data to the Garnet-biotite Geothermometer[J].American Mineralogist,2000,85(7/8):881-892.
[61] FLORENCE F P,SPEAR F S.Intergranular Diffusion Kinetics of Fe and Mg During Retrograde Metamorphism of a Pelitic Gneiss from the Adirondack Mountains[J].Earth and Planetary Science Letters,1995,134(3):329-340.
[62] O’BRIEN P J.Asymmetric Zoning Profiles in Garnet from HP-HT Granulite and Implications for Volume and Grain-boundary Diffusion[J].Mineralogical Maga-zine,1999,63(2):227-238.
[63] WU C M,ZHAO G C.Recalibration of the Garnet-muscovite(GM)Geothermometer and the Garnet-muscovite-plagioclase-quartz(GMPQ)Geobarometer for Metapelitic Assemblages[J].Journal of Petrology,2006,47(12):2357-2368.
[64] 朱新人.东秦岭武当山地区晚前寒武纪地层成岩构造环境及其后期地质演化[D].北京:中国科学院地质与地球物理研究所,1988.
ZHU Xin-ren.The Structural Environment and Later Geological Evolution of Stratum Diagenesis in Wudang District of East Qinling in Precambrian Era[D].Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences,1988.
[65] 胡健民,马国良,高殿松,等.武当地块主要地质事件年代学研究[J].中国区域地质,2000,19(3):318-324.
HU Jian-min,MA Guo-liang,GAO Dian-song,et al.Chronology of Major Geological Events of the Wudang Block in the South Qinling Orogeny[J].Regional Geology of China,2000,19(3):318-324.
[66] 王 刚,张 晗,王宗起,等.武当山十堰地区二叠纪E-MORB型玄武岩识别及构造意义[J].地质论评,2019,65(1):65-85.
WANG Gang,ZHANG Han,WANG Zong-qi,et al.Identification of the Permian E-MORB Type Basalts and Their Tectonic Significance from Shiyan Area,Wudang Mountain[J].Geological Review,2019,65(1):65-84.
[67] 张国伟,张本仁,袁学诚.秦岭造山带与大陆动力学[M].北京:科学出版社,2001.
ZHANG Guo-wei,ZHANG Ben-ren,YUAN Xue-cheng,et al.Qinling Orogenic Belt and Continental Dynamics[M].Beijing:Science Press,2001.
[68] 凌文黎,程建萍,王歆华,等.武当地区新元古代岩浆岩地球化学特征及其对南秦岭晋宁期区域构造性质的指示[J].岩石学报,2002,18(1):25-36.
LING Wen-li,CHENG Jian-ping,WANG Xin-hua,et al.Geochemical Features of the Neoproterozoic Igneous Rocks from the Wudang Region and Their Implications for the Reconstruction of the Jinning Tectonic Evolution Along the South Qinling Orogenic Belt[J].Acta Petrologica Sinica,2002,18(1):25-36.
[69] 卢山松,江 拓,彭三国,等.武当地块与扬子陆核区新元古代早期沉积岩碎屑锆石U-Pb年代学对比及其地质意义[J].岩石矿物学杂志,2017,36(5):646-654.
LU Shan-song,JIANG Tuo,PENG San-guo,et al.Comparison of Detrital Zircon U-Pb Geochronology Between the Wudang Block and the Yangtze Continental Nucleus in Terms of Neorproterozoic Sedimentary Rocks[J].Acta Petrologica et Mineralogica,2017,36(5):646-654.
[70] 许 光,王 刚,王宗起,等.武当山南缘房县地区早古生代镁铁质岩石成因及大地构造意义[J].地球学报,2018,39(3):306-321.
XU Guang,WANG Gang,WANG Zong-qi.et al.Petrogenesis of the Early Paleozoic Mafic Rock in Fangxian Area on the Southern Margin of Wudang Mountain and Its Tectonic Significance[J].Acta Geoscientica Sinica,2018,39(3):306-321.
[71] 王 刚,王宗起,武昱东,等.武当山腹地晚古生代沉积与火山物质的识别:微体化石和锆石年代学证据[J].地质学报,2018,92(6):1163-1175.
WANG Gang,WANG Zong-qi,WU Yu-dong,et al.The Determination of Late Paleozoic Volcanic and Sedimentary Substances in the Hinterland of Wudang Mountain,South Qinling Orogeny:Evidence from Microfossil and Zircon Geochronology[J].Acta Geologica Sinica,2018,92(6):1163-1175.
[72] 蔡志勇,罗 洪,熊小林,等.武当群上部变沉积岩组时代归属问题:单锆石U-Pb年龄的制约[J].地层学杂志,2006,30(1):60-63.
CAI Zhi-yong,LUO Hong,XIONG Xiao-lin,et al.A Discussion on the Age of the Meta-sedimentary Rocks in the Upper Part of the Wudang Group:Constrained by the Grain-zircon U-Pb Dating[J].Journal of Stratigraphy,2006,30(1):60-63.
[73] 周高志,高敬礼,康维国,等.鄂北蓝片岩带若干问题讨论[J].中国区域地质,1990(3):255-261.
ZHOU Gao-zhi,GAO Jing-li,KANG Wei-guo,et al.Several Problems on the Blueschist Belt in Northern Hubei[J].Regional Geology of China,1990(3):255-261.
[74] SEBASTIAN W,SASCHA S,IRENA M,et al.Dating the Initiation of Piemonte-Liguria Ocean Subduction:Lu-Hf Garnet Chronometry of Eclogites from the Theodul Glacier Unit(Zermatt-Saas Zone,Switzerland)[J].Swiss Journal of Geosciences,2015,108(2/3):183-199.
[75] WAKABAYASHI J.Subducted Sedimentary Serpentinite MeLanges:Record of Multiple Burial-exhumation Cycles and Subduction Erosion[J].Tectonophysics,2012,568/569:230-247.
[76] WAKITA K.Mappable Features of MeLanges Derived from Ocean Plate Stratigraphy in the Jurassic Accretionary Complexes of Mino and Chichibu Terranes in Southwest Japan[J].Tectonophysics,2012,568/569:74-85.
[77] PEIXOTO E,PEDROSA-SOARES A C,ALKMIM F F,et al.A Suture-related Accretionary Wedge Formed in the Neoproterozoic Aracuai Orogen(SE Brazil)During Western Gondwanaland Assembly[J].Gondwana Research,2015,27:878-896.
[78] 李林贵,梁 晓,王根厚,等.西藏羌塘增生杂岩带内中—晚三叠世碳酸盐岩地层的发现及大地构造意义[J].地质学报,2018,92(4):828-844.
LI Lin-gui,LIANG Xiao,WANG Gen-hou,et al.Discovery of the Middle-Late Triassic Carbonatite Formation in the Central Qiangtang Accretionary Complex,North Tibet and Its Tectonic Siginifiance[J].Acta Geologica Sinica,2018,92(4):828-844.

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备注/Memo

备注/Memo:
收稿日期:2019-03-04; 修回日期:2019-05-20投稿网址:http://jese.chd.edu.cn/
基金项目:国家重点研发计划项目(2016YFC0600202); 国家自然科学基金项目(41702213,41702076); 中国地质科学院基本科研业务费专项资金项目(K1614)
作者简介:王东升(1988-),男,河南濮阳人,助理研究员,理学博士,E-mail:wangdsyzy@126.com。
*通讯作者:王宗起(1960-),男,天津市人,研究员,博士研究生导师,理学博士,E-mail:wzq@ccsd.org.cn。
更新日期/Last Update: 2019-07-11