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南海及其围区新生代岩浆活动时序与成因研究

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谢安远, 钟立峰, 颜文. 南海及其围区新生代岩浆活动时序与成因研究[J]. 海洋地质与第四纪地质, 2017, 37(2): 108-118. doi: 10.16562/j.cnki.0256-1492.2017.02.011
引用本文: 谢安远, 钟立峰, 颜文. 南海及其围区新生代岩浆活动时序与成因研究[J]. 海洋地质与第四纪地质, 2017, 37(2): 108-118. doi: 10.16562/j.cnki.0256-1492.2017.02.011
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XIE Anyuan, ZHONG Lifeng, YAN Wen. TIMING AND GENESIS OF CENOZOIC MAGMATISMS IN THE SOUTH CHINA SEA AND SURROUNDING AREAS[J]. Marine Geology & Quaternary Geology, 2017, 37(2): 108-118. doi: 10.16562/j.cnki.0256-1492.2017.02.011
Citation: XIE Anyuan, ZHONG Lifeng, YAN Wen. TIMING AND GENESIS OF CENOZOIC MAGMATISMS IN THE SOUTH CHINA SEA AND SURROUNDING AREAS[J]. Marine Geology & Quaternary Geology, 2017, 37(2): 108-118. doi: 10.16562/j.cnki.0256-1492.2017.02.011
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南海及其围区新生代岩浆活动时序与成因研究

  • 1.

    中国科学院南海海洋研究所，中国科学院边缘海与大洋地质重点实验室，广州 510301

  • 2.

    中国科学院大学，北京 100049

  • 3.

    中山大学海洋科学学院，广州 510006

  • 基金项目:
    同位素地球化学国家重点实验室(中国科学院广州地球化学研究所)项目(SKLIG-KF-14-08)；广东省自然科学基金项目(2015A030313836)
详细信息
    作者简介: 谢安远(1992-)，男，硕士研究生，从事海洋地球化学研究。E-mail：ayxie@scsio.ac.cn
    通讯作者: 钟立峰。E-mail: zhonglf@scsio.ac.cn

  • 中图分类号: P736.1

    • 文凤英编辑

TIMING AND GENESIS OF CENOZOIC MAGMATISMS IN THE SOUTH CHINA SEA AND SURROUNDING AREAS

  • 1.

    CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

  • 2.

    University of Chinese Academy of Sciences, Beijing 100049, China

  • 3.

    School of Marine Sciences, Sun Yat-Sen University, Guangzhou 510006, China

More Information

    摘要

  • 南海及其围区新生代岩浆活动具有相似的特征，根据与南海扩张时间(32~15.5 Ma)的先后关系，将岩浆活动分为三期：扩张前(>32 Ma)、扩张期(32~15.5 Ma)和停止扩张后(< 15.5 Ma)。从岩相学特征可知：扩张前的岩石以三水盆地双峰式岩浆岩组合为代表；根据最新的IODP 349航次的钻孔样品资料，南海海盆扩张期岩浆岩为典型的MORB，而少量的陆缘岩石资料显示，该期岩浆岩为碱性玄武岩；停止扩张后岩浆活动可分为两期，早期以大陆-大洋中脊过渡型拉斑玄武岩为主，晚期以碱性玄武岩为主。除了扩张期南海海盆的MORB，整个新生代的岩浆岩地球化学特征大体一致，与OIB相似，显示地幔源区具有不均一性，由一个DMM和一个EM端元组成，且岩石均表现出明显的Dupal异常特征。对于富集端元的性质和来源、Dupal异常的成因、海南地幔柱是否存在等问题目前存在较大争议。具OIB特征的岩浆除来自地幔柱作用外，地幔交代作用也是重要的产生机制。本文认为碳酸盐流体对地幔源区的交代作用可能在南海地区新生代岩浆活动中扮演了重要的角色。另外，岩浆岩成岩过程的研究也不够全面深入，这些都是在今后的研究工作中需要关注的地方，有待后来进一步的研究。

    The Cenozoic magmatic activities in the South China Sea (SCS) are similar with its surrounding areas. It may be divided into three stages following the spreading of the SCS: pre-spreading (32 Ma), syn-spreading (32~15.5 Ma), and post-spreading (< 15.5 Ma). The pre-spreading rocks are bimodal volcanic rock suite which is typically exposed in the Sanshui basin; the syn-spreading magmatic rocks in the SCS basin are typical MORB according to the data from IODP expedition 349, but the limited syn-spreading magmatic rocks in eastern Guangdong and western Taiwan are alkali basalts; the post-spreading magmatism can be subdivided into two periods: the early period dominated by tholeiites and the late predominated by alkali basalts. The geochemical characteristics of the Cenozoic magmatic rocks (expect the syn-spreading MORB) in the SCS and its surrounding areas are consistent and similar with OIB, indicating that the mantle source is heterogeneous, which is composed of a DMM and an EM end member, and show the Dupal isotope anomaly. However, there are controversies in the issues such as the nature and origin of the EM end member, cause of the Dupal isotope anomaly, and the existence of the Hainan plume. The plume may produce OIB-like magmas, but not all OIB-like magmas are produced from the plume, mantle metasomatism can also have important impact on the magmatism. In this paper, it's considered that carbonate fluids metasomatism in the mantle source may play an important role in the Cenozoic magmatism in the SCS and its surrounding areas. The research on the diagenetic process is not enough yet. These are the places where attention needs to be paid to in the future research work.

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  • 图 1  南海及其围区新生代岩浆岩分布简图(据文献[43]修改)

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  南海及其围区新生代岩浆岩年龄分布(数据来源同表 2)

    Figure 2. 

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    图 3  南海及其围区新生代岩浆岩微量元素蛛网图(左)和REE配分曲线(右)

    Figure 3. 

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    图 4  南海及围区新生代岩浆岩同位素相关图解

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    表 1  南海扩张时间

    Table 1.  Opening time of the South China Sea

    研究区域 扩张时间/Ma 数据来源
    东部次海盆 32~16 文献[1, 2]
    中央海盆 32~17 文献[3]
    西南次海盆 42~35 (文献[6])
    中央海盆 31~20.5 (文献[11])
    西南次海盆 31~20.5 (文献[12])
    中部和东北海盆 37~15 文献[5]
    东部次海盆 33~16 文献[4]
    西南次海盆 起始时间：23.6~21.5 文献[4]
    结束时间：15
    下载: 导出CSV

    表 2  南海及其围区新生代岩浆岩年龄

    Table 2.  Ages of Cenozoic magmatic rocks in the SCS and its surrounding areas

    分期 地区 岩性 年龄/Ma 测年方法 数据来源
    扩张前 三水盆地 粗面岩、流纹岩、玄武岩 43~64 K-Ar 文献[13]
    台湾西部 玄武岩、英安岩、流纹岩 37.7~53.7 Ar-Ar 文献[18]
    珠江口盆地 玄武岩、粗面岩、英安岩、安山岩、流纹岩 33.6~51.6 K-Ar 文献[14]
    扩张期 粤东普寨和韭菜地 碱性玄武岩 20.2~20.8 Ar-Ar 文献[17]
    台湾西北部 碱性玄武岩 20~23 文献[21]
    台湾西南部 碱性玄武岩 21~22.1 Ar-Ar 文献[19]
    双峰海山 粗面岩 23.3~23.8 Ar-Ar 文献[20]
    宪北海山 碱性和拉斑玄武岩 15~38 文献[24]
    停止扩张后 中南海山 碱性玄武岩 3.49 稀释法 文献[22]
    珍贝海山 拉斑玄武岩 9.5 稀释法 文献[22]
    黄岩海山 粗面岩 7.77 K-Ar 文献[39]
    涨中海山 碱性玄武岩 4.76~5.78 K-Ar 文献[36]
    玳瑁海山 拉斑玄武岩 14.1 稀释法 文献[22]
    玄武质火山角砾岩 16.6 K-Ar 文献[42]
    海南岛 碱性和拉斑玄武岩 0.68~12.89 Ar-Ar 文献[40]
    雷琼地区 碱性和拉斑玄武岩 0.18~4.13 Ar-Ar 文献[30]
    北部湾 玄武岩 1.1~5.9 K-Ar 文献[33]
    越南 碱性和拉斑玄武岩 0.4~15.5 Ar-Ar 文献[29]
    下载: 导出CSV
    • 参考文献(66)
  • [1]

    Taylor B, Hayes D E. The tectonic evolution of the South China Basin [J]. Washington Dc American Geophysical Union Geophysical Monograph, 1980, 23:89-104. http://onlinelibrary.wiley.com/doi/10.1029/GM023p0089/pdf

    [2]

    Taylor B, Hayes D E. Origin and history of the South China Sea basin [J]. Washington Dc American Geophysical Union Geophysical Monograph, 1983, 27:23-56. http://onlinelibrary.wiley.com/doi/10.1029/GM027p0023/pdf

    [3]

    Briais A, Patriat P, Tapponnier P. Updated interpretation of magnetic-anomalies and sea-floor spreading stages in the South China Sea-implications for the tertiary tectonics of southeast-asia [J]. Journal of Geophysical Research-Solid Earth, 1993, 98(B4): 6299-6328. doi: 10.1029/92JB02280

    [4]

    Li C-F, Xu X, Lin J, et al. Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349 [J]. Geochemistry Geophysics Geosystems, 2014, 15(12): 4958-4983. doi: 10.1002/2014GC005567

    [5]

    Hsu S K, Yeh Y C, Doo W B, et al. New bathymetry and magnetic lineations identifications in the northernmost South China Sea and their tectonic implications [J]. Marine Geophysical Researches, 2004, 25(1-2): 29-44. doi: 10.1007/s11001-005-0731-7

    [6]

    姚伯初.中美合作调研南海地质专报[M].中国地质大学出版社, 1994.

    YAO Bochu. The Geological Memoir of South China Sea Surveyed Jointly by China & USA[M].China Unversity of Geosciences Press, 1994.

    [7]

    Karig D E. Origin and Development of Marginal Basins in the Western Pacific [J]. Journal of Geophysical Research Atmospheres, 1971, 76(11): 2542-2561. doi: 10.1029/JB076i011p02542

    [8]

    Tapponnier P, Peltzer G, Armijo R. On the mechanics of the collision between India and Asia [J]. Geological Society London Special Publications, 1986, 19(1): 113-157. doi: 10.1144/GSL.SP.1986.019.01.07

    [9]

    李思田, 林畅松.南海北部大陆边缘盆地幕式裂隙的动力过程及10Ma以来的构造事件[J].科学通报, 1998(8): 797-810. doi: 10.3321/j.issn:0023-074X.1998.08.003

    LI Sitian, LIN Changsong. Dynamic processes of episodic fissures in the continental margin basin of the northern continental margin of the South China Sea and tectonic events since 10Ma[J]. Chinese Science Bulletin, 1998(8):797-810. doi: 10.3321/j.issn:0023-074X.1998.08.003

    [10]

    李家彪, 金翔龙, 高金耀.南海东部海盆晚期扩张的构造地貌研究[J].中国科学, 2002, 32(3): 239-248. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200203009

    LI Jiabiao, JIN Xianglong, GAO Jinyao. Tectonic landform of the late expansion in the eastern South China Sea basin[J]. Science in China(Series D), 2002, 32(3):239-248. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200203009

    [11]

    Barckhausen U, Roeser H A. Seafloor spreading anomalies in the South China Sea revisited [J]. Continent-Ocean Interactions Within East Asian Marginal Seas, 2004, 149:121-125. http://adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004GMS...149..121B&db_key=PHY&link_type=ABSTRACT

    [12]

    Barckhausen U, Engels M, Franke D, et al. Evolution of the South China Sea: Revised ages for breakup and seafloor spreading [J]. Marine and Petroleum Geology, 2014, 58:599-611. doi: 10.1016/j.marpetgeo.2014.02.022

    [13]

    朱炳泉, 王慧芬.雷琼地区MORB-OIB过渡型地幔源火山作用的Nd-Sr-Pb同位素证据[J].地球化学, 1989(3):193-201. doi: 10.3321/j.issn:0379-1726.1989.03.001

    ZHU Bingquan, WANG Huifen. Nd-Sr-Pb isotopic and chemical evidence for the volcanism with MORB-OIB source characteristics in the Leiqiong area, China[J]. Geochemica, 1989(3):193-201. doi: 10.3321/j.issn:0379-1726.1989.03.001

    [14]

    邹和平.试谈南海海盆地壳属性问题——由南海海盆及其邻区玄武岩的比较研究进行讨论[J].大地构造与成矿学, 1993(4):293-303. http://www.cnki.com.cn/Article/CJFD1993-DGYK199304000.htm

    ZOU Heping. On the problem about the crust′s attribution of South China Sea basin-discussion from comparative study on basalts of seamounts in South China Sea basin and the neighboring areas[J]. Geotectonica et Metallogenia, 1993(4):293-303. http://www.cnki.com.cn/Article/CJFD1993-DGYK199304000.htm

    [15]

    Chung S L, Cheng H, Jahn B M, et al. Major and trace element, and Sr-Nd isotope constraints on the origin of Paleogene volcanism in South China prior to the South China Sea opening [J]. Lithos, 1997, 40(2-4): 203-220. doi: 10.1016/S0024-4937(97)00028-5

    [16]

    肖龙, 周海民, 董月霞, 等.广东三水盆地火山岩:地球化学特征及成因——兼论火山岩性质的时空演化和南海形成的深部过程[J].大地构造与成矿学, 2006, 30(1): 72-81. doi: 10.3969/j.issn.1001-1552.2006.01.009

    XIAO Long, ZHOU Haimin, DONG Yuexia, et al. Geochemistry and petrogenesis of cenozoic volcanic rocks from Sanshui basin: implications for spatial and temporal variation of rock types and constraints on the formation of South China Sea[J]. Geotectonica et Metallogenia, 2006, 30(1):72-81. doi: 10.3969/j.issn.1001-1552.2006.01.009

    [17]

    Huang X L, Niu Y L, Xu Y G, et al. Geochronology and geochemistry of Cenozoic basalts from eastern Guangdong, SE China: constraints on the lithosphere evolution beneath the northern margin of the South China Sea [J]. Contributions to Mineralogy and Petrology, 2013, 165(3): 437-455. doi: 10.1007/s00410-012-0816-7

    [18]

    Wang K-L, Chung S-L, Lo Y-M, et al. Age and geochemical characteristics of Paleogene basalts drilled from western Taiwan: Records of initial rifting at the southeastern Eurasian continental margin [J]. Lithos, 2012, 155:426-441. doi: 10.1016/j.lithos.2012.10.002

    [19]

    Wang K-L, Lo Y-M, Chung S-L, et al. Age and geochemical features of dredged basalts from offshore SW Taiwan: The coincidence of intra-plate magmatism with the spreading South China Sea [J]. Terrestrial Atmospheric and Oceanic Sciences, 2012, 23(6): 657-669. doi: 10.3319/TAO.2012.07.06.01(TT)

    [20]

    Li X, Li J, Yu X, et al. 40Ar/39Ar ages of seamount trachytes from the South China Sea and implications for the evolution of the northwestern sub-basin [J]. Geoscience Frontiers, 2015, 149(4): 571-577. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy-e201504008

    [21]

    Chung S L, Jahn B M, Chen S J, et al. Miocene basalts in northwestern taiwan - evidence for Em-type mantle sources in the continental lithosphere [J]. Geochimica et Cosmochimica Acta, 1995, 59(3): 549-555. doi: 10.1016/0016-7037(94)00360-X

    [22]

    王贤觉, 吴明清, 梁德华, 等.南海玄武岩的某些地球化学特征[J].地球化学, 1984(4): 332-340. doi: 10.3321/j.issn:0379-1726.1984.04.005

    WANG Xianjue, WU Mingqing, LIANG Dehua, et al. Some geochemical characteristics of basalts in the South China Sea[J]. Geochemica, 1984(4):332-340. doi: 10.3321/j.issn:0379-1726.1984.04.005

    [23]

    Kan T, Flower M F J, Carlson R W, et al. Sr, Nd, and Pb isotopic compositions of Hainan basalts (South China) - implications for a subcontinental lithosphere Dupal source [J]. Geology, 1991, 19(6): 567-569. doi: 10.1130/0091-7613(1991)019<0567:SNAPIC>2.3.CO;2

    [24]

    李兆麟, 丘志力, 秦社彩, 等.南海海山玄武岩形成条件研究[J].矿物学报, 1991(4): 325-333. doi: 10.3321/j.issn:1000-4734.1991.04.005

    LI Zhaolin, QIU Zhili, QIN Shecai, et al. A study of the forming conditions of basalts in seamounts of the South China Sea[J]. Acta Mineralogica Sincia, 1991(4):325-333. doi: 10.3321/j.issn:1000-4734.1991.04.005

    [25]

    Flower M F J, Zhang M, Chen C Y, et al. Magmatism in the South China Basin.2. post-spreading quaternary basalts from Hainan island, South China [J]. Chemical Geology, 1992, 97(1-2): 65-87. doi: 10.1016/0009-2541(92)90136-S

    [26]

    Tu K, Flower M F J, Carlson R W, et al. Magmatism in the South China basin.1. isotopic and trace-element evidence for an endogenous dupal mantle component [J]. Chemical Geology, 1992, 97(1-2): 47-63. doi: 10.1016/0009-2541(92)90135-R

    [27]

    Chung S L, Sun S S, Tu K, et al. Late cenozoic basaltic volcanism around the Taiwan Strait, SE China - product of lithosphere asthenosphere interaction during continental extension [J]. Chemical Geology, 1994, 112(1-2): 1-20. doi: 10.1016/0009-2541(94)90101-5

    [28]

    Nguyen H, Flower M F J, Carlson R W. Major, trace element, and isotopic compositions of Vietnamese basalts: Interaction of hydrous EM1-rich asthenosphere with thinned Eurasian lithosphere [J]. Geochimica et Cosmochimica Acta, 1996, 60(22): 4329-4351. doi: 10.1016/S0016-7037(96)00247-5

    [29]

    Hoang N, Flower M. Petrogenesis of Cenozoic basalts from Vietnam: Implication for origins of a diffuse igneous province′ [J]. Journal of Petrology, 1998, 39(3): 369-395. doi: 10.1093/petroj/39.3.369

    [30]

    Ho K S, Chen J C, Juang W S. Geochronology and geochemistry of late Cenozoic basalts from the Leiqiong area, Southern China [J]. Journal of Asian Earth Sciences, 2000, 18(3): 307-324. doi: 10.1016/S1367-9120(99)00059-0

    [31]

    Zou H, Zindler A, Xu X, et al. Major, trace element, and Nd, Sr and Pb isotope studies of Cenozoic basalts in SE China: mantle sources, regional variations, and tectonic significance [J]. Chemical Geology, 2000, 171(1-2): 33-47. doi: 10.1016/S0009-2541(00)00243-6

    [32]

    Yumul G P, Dimalanta C B, Tamayo R A, et al. Silicic arc volcanism in Central Luzon, the Philippines: Characterization of its space, time and geochemical relationship [J]. Island Arc, 2003, 12(2): 207-218. doi: 10.1046/j.1440-1738.2003.00393.x

    [33]

    贾大成, 丘学林, 胡瑞忠, 等.北部湾玄武岩地幔源区性质的地球化学示踪及其构造环境[J].热带海洋学报, 2003, 22(2):30-39. doi: 10.3969/j.issn.1009-5470.2003.02.004

    JIA Dacheng, QIU Xuelin, HU Ruizhong, et al. Geochemical nature of mantle reservoirs and tectonic setting of basalts in Beibu gulf and its adjacent region[J]. Journal of Tropical Oceanography, 2003, 22(2):30-39. doi: 10.3969/j.issn.1009-5470.2003.02.004

    [34]

    李昌年, 王方正, 钟称生.广西北海涠洲岛(含斜阳岛)第四纪玄武质火山岩的地球化学性质及其源区特征[J].岩石矿物学杂志, 2005, 24(1):1-11. doi: 10.3969/j.issn.1000-6524.2005.01.001

    LI Changnian, WANG Fangzheng, ZHONG Chengsheng. Geochemistry of Quaternary basaltic volcanic rocks of Weizhou island in Beihai City of Guangxi and a discussion on characteristics of their source[J]. Acta Petrologica Et Mineralogica, 2005, 24(1):1-11. doi: 10.3969/j.issn.1000-6524.2005.01.001

    [35]

    樊祺诚, 孙谦, 隋建立, 等.北部湾涠洲岛及斜阳岛火山岩微量元素和同位素地球化学及其构造意义[J].岩石学报, 2008, 24(6):1323-1332. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200806015

    FAN Qicheng, SUN Qian, SUI Jianli, et al. Trace element and isotopic geochemistry of volcanic rocks and its tectonic implications in Weizhou Island and Xieyang Island, Nortern Bay[J]. Acta Petrologica Sinica, 2008, 24(6):1323-1332. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200806015

    [36]

    鄢全树, 石学法, 王昆山, 等.南海新生代碱性玄武岩主量、微量元素及Sr-Nd-Pb同位素研究[J].中国科学(D辑:地球科学), 2008(1): 56-71. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd200801006

    YAN Quanshu, SHI Xuefa, WANG Kunshan, et al. Study on the major, trace element and Sr-Nd-Pb isotope of cenozoic alkali basalts from the South China Sea[J]. Science in China(Series D), 2008(01):56-71. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd200801006

    [37]

    Zhou H M, Xiao L, Dong Y X, et al. Geochemical and geochronological study of the Sanshui basin bimodal volcanic rock suite, China: Implications for basin dynamics in southeastern China [J]. Journal of Asian Earth Sciences, 2009, 34(2): 178-189. doi: 10.1016/j.jseaes.2008.05.001

    [38]

    韩江伟, 熊小林, 朱照宇.雷琼地区晚新生代玄武岩地球化学:EM2成分来源及大陆岩石圈地幔的贡献[J].岩石学报, 2009, 25(12): 3208-3220. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200912009

    HAN Jiangwei, XIONG Xiaolin, ZHU Zhaoyu. Geochemistry of Late-Cenozoic basalts from Leiqiong area: The origin of EM2 and the contribution from sub-continental lithosphere mantle[J].Acta Petrologica Sinica, 2009, 25(12):3208-3220. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200912009

    [39]

    王叶剑, 韩喜球, 罗照华, 等.晚中新世南海珍贝-黄岩海山岩浆活动及其演化:岩石地球化学和年代学证据[J].海洋学报(中文版), 2009, 31(4):93-102. doi: 10.3321/j.issn:0253-4193.2009.04.011

    WANG Yejian, HAN Xiqiu, LUO Zhaohua, et al. Late Miocene magmatism and evolution of Zhenbei-Huangyan Seamount in the South China Sea:Evidence from petrochemistry and chronology[J]. Acta Oceanologica Sinica, 2009, 31(4):93-102. doi: 10.3321/j.issn:0253-4193.2009.04.011

    [40]

    Wang X C, Li Z X, Li X H, et al. Temperature, pressure, and composition of the mantle source region of Late Cenozoic basalts in Hainan Island, SE Asia: a consequence of a young thermal mantle plume close to subduction zones? [J]. Journal of Petrology, 2012, 53(1): 177-233. doi: 10.1093/petrology/egr061

    [41]

    Li N, Yan Q, Chen Z, et al. Geochemistry and petrogenesis of Quaternary volcanism from the islets in the eastern Beibu Gulf: evidence for Hainan plume [J]. Acta Oceanologica Sinica, 2013, 32(12): 40-49. doi: 10.1007/s13131-013-0386-1

    [42]

    Yan Q, Castillo P, Shi X, et al. Geochemistry and petrogenesis of volcanic rocks from Daimao Seamount (South China Sea) and their tectonic implications [J]. Lithos, 2015, 218-219:117-126. doi: 10.1016/j.lithos.2014.12.023

    [43]

    徐义刚, 魏静娴, 邱华宁, 等.用火山岩制约南海的形成演化:初步认识与研究设想[J].科学通报, 2012, 57(20):1863-1878. http://www.cnki.com.cn/Article/CJFDTotal-KXTB201220006.htm

    XU Yigang, WEI Jingxian, QIU Huaning, et al. Opening and evolution of the South China Sea constrained by studies on volcanic rocks: Preliminary results and a research design[J]. Chinese Science Bulletin, 2012, 57(20):1863-1878. http://www.cnki.com.cn/Article/CJFDTotal-KXTB201220006.htm

    [44]

    Expedition 349 Scientists. South China Sea tectonics: Opening of the South China Sea and its implications for southeast Asian tectonics, climates, and deep mantle processes since the late Mesozoic[R]. International Ocean Discovery Program Preliminary Report, 349, 2014.

    [45]

    Sun S S, Mcdonough W F. Chemical and isotopic systematics of oceanic basalts; Implications for mantle composition and processes[J]. Geological Society London Special Publications, 1989, 42(1):313-345. doi: 10.1144/GSL.SP.1989.042.01.19

    [46]

    Hart S R. A large-scale isotope anomaly in the Southern Hemisphere mantle [J]. Nature, 1984, 309(5971): 753-757. doi: 10.1038/309753a0

    [47]

    Zindler A, Hart S. Chemical Geodynamics[J]. Annual Review of Earth & Planetary Sciences, 2003, 14(1):493-571. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200101011

    [48]

    Mahoney J J, Natland J H, White W M, et al. Isotopic and geochemical provinces of the western Indian Ocean Spreading Centers [J]. Journal of Geophysical Research Atmospheres, 1989, 94(B4): 4033-4052. doi: 10.1029/JB094iB04p04033

    [49]

    邹和平, 李平鲁, 饶春涛.珠江口盆地新生代火山岩地球化学特征及其动力学意义[J].地球化学, 1995(S1): 33-45. http://www.cqvip.com/qk/92960X/1995C00/11005254.html

    ZOU Heping, LI Pinglu, RAO Chuntao. Geochemistry of Cenozoic volcanic rocks in Zhujiangkou basin and its geodynamic significance[J]. Geochemica, 1995(S1):33-45. http://www.cqvip.com/qk/92960X/1995C00/11005254.html

    [50]

    杨蜀颖, 方念乔, 杨胜雄, 等.关于南海中央次海盆海山火山岩形成背景与构造约束的再认识[J].地球科学:中国地质大学学报, 2011, 36(3):455-470. http://d.old.wanfangdata.com.cn/Periodical/dqkx201103005

    YANG Shuying, FANG Nianqiao, YANG Shengxiong, et al. A further discussion on formation background and tectonic constraints of igneous rocks in central sub-basin of the South China Sea[J]. Earth Science-Journal of China University of Geosciences, 2011, 36(3):455-470. http://d.old.wanfangdata.com.cn/Periodical/dqkx201103005

    [51]

    任江波, 王嘹亮, 鄢全树, 等.南海玳瑁海山玄武质火山角砾岩的地球化学特征及其意义[J].地球科学:中国地质大学学报, 2013(S1):10-20. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=8632487

    REN Jiangbo, WANG Liaoliang, YAN Quanshu, et al. Geochemical characteristics and its geological implications for basalts in volcaniclastic rock from daimao seamount[J]. Earth Science-Journal of China University of Geosciences, 2013(S1):10-20. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=8632487

    [52]

    邢光福. Dupal同位素异常的概念、成因及其地质意义[J].火山地质与矿产, 1997(4): 281-291. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700247320

    XING Guangfu. The Dupal isotope anomaly: its concept, character, genesis and geological significance[J]. Volcanology & Mineral Resources, 1997(4):281-291. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700247320

    [53]

    Hawkesworth C J, Mantovani M S M, Taylor P N, et al. Evidence from the Parana of south Brazil for a continental contribution to Dupal basalts [J]. Nature, 1986, 322(6077): 356-359. doi: 10.1038/322356a0

    [54]

    Burdick J. Osmium isotopic constraints on the nature of the DUPAL anomaly from Indian mid-ocean-ridge basalts [J]. Nature, 2004, 431(7004): 59-63. doi: 10.1038/nature02904

    [55]

    Mukasa S B, Mccabe R, Gill J B. Pb-isotopic compositions of volcanic rocks in the West and East Philippine island arcs: presence of the Dupal isotopic anomaly [J]. Earth & Planetary Science Letters, 1987, 84(2-3): 153-164. http://www.sciencedirect.com/science/article/pii/0012821X87900823

    [56]

    Tatsumoto M, Nakamura Y. DUPAL anomaly in the Sea of Japan: Pb, Nd, and Sr isotopic variations at the eastern Eurasian continental margin [J]. Geochimica et Cosmochimica Acta, 1991, 55(12): 3697-3708. doi: 10.1016/0016-7037(91)90068-G

    [57]

    钟立峰, 夏斌, 周国庆, 等.藏南罗布莎蛇绿岩成因:壳层熔岩的Sr-Nd-Pb同位素制约[J].矿物岩石, 2006, 26(1):57-63. doi: 10.3969/j.issn.1001-6872.2006.01.011

    ZHONG Lifeng, XIA Bin, ZHOU Guoqing, et al. Origin of the Luobusa ophiolite, southern Tibet: Sr-Nd-Pb isotopic constraints on crust lavas[J]. J. Mineral Petrol., 2006, 26(1):57-63. doi: 10.3969/j.issn.1001-6872.2006.01.011

    [58]

    Ridd M F. South-East Asia as a part of Gondwanaland [J]. Nature, 1971, 234(5331): 531-533. doi: 10.1038/234531a0

    [59]

    Lin J L, Fuller M, Zhang W Y. Preliminary phanerozoic polar wander paths for the North and South China blocks [J]. Nature, 1985, 313(6002): 444-449. doi: 10.1038/313444a0

    [60]

    Nie S Y. Constraints on the locations of Asian microcontinents in Palaeo Tethys during the Late Palaezoic [J]. Palaeozoic Palaeogeography & Biogeography, 1990:397-409. http://www.onacademic.com/detail/journal_1000034835644310_8d1f.html

    [61]

    朱永峰.地幔流体与地球的放气作用[J].地学前缘, 1998(S1): 71-75. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy1998z1006

    ZHU Yongfeng. Mantle fluid and earth degassing[J]. Earth Science Frontiers, 1998(S1):71-75. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy1998z1006

    [62]

    Dasgupta R, Hirschmann M M, Smith N D. Partial melting experiments of peridotite + CO2 at 3 GPa and genesis of alkalic ocean island basalts [J]. Journal of Petrology, 2007, 48(11): 2093-2124. doi: 10.1093/petrology/egm053

    [63]

    Hofmann A W. Mantle geochemistry: The message from oceanic volcanism [J]. Nature, 1997, 385(6613): 219-229. doi: 10.1038/385219a0

    [64]

    Burton K W, Gannoun A, Birck J L, et al. The compatibility of rhenium and osmium in natural olivine and their behaviour during mantle melting and basalt genesis [J]. Earth and Planetary Science Letters, 2002, 198(1-2): 63-76. doi: 10.1016/S0012-821X(02)00518-6

    [65]

    Bockrath C, Ballhaus C, Holzheid A. Fractionation of the platinum-group elements during mantle melting [J]. Science, 2004, 305(5692): 1951-1953. doi: 10.1126/science.1100160

    [66]

    Lorand J P, Luguet A, Alard O. Platinum-group elements: A new set of key tracers for the earth′s interior [J]. Elements, 2008, 4(4): 247-252. doi: 10.2113/GSELEMENTS.4.4.247

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