Article(id=1242138620526670147, tenantId=1146029695717560320, journalId=1146031591421210625, issueId=1242138608648397669, articleNumber=null, orderNo=7, doi=10.3981/j.issn.1000-7857.2020.18.005, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1589126400000, receivedDateStr=2020-05-11, revisedDate=1592496000000, revisedDateStr=2020-06-19, acceptedDate=null, acceptedDateStr=null, onlineDate=1604479741707, onlineDateStr=2020-11-04, pubDate=1601222400000, pubDateStr=2020-09-28, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1604479741707, onlineIssueDateStr=2020-11-04, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1774078524949, creator=sys-migrate, updateTime=1774078524949, updator=sys-migrate, issue=Issue{id=1242138608648397669, tenantId=1146029695717560320, journalId=1146031591421210625, year='2020', volume='38', issue='18', pageStart='1', pageEnd='104', issueExtLink='null', onlineDate='null', pubDate='1601222400000', pubDateStr='2020-09-28', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=3, issueType=-1, specialIssue=null, createTime=1774078522118, creator='sys-migrate', updateTime=1774078522118, updator='sys-migrate', preIssue=null, nextIssue=null, articleTotal=null, ext=null, issueFiles=null, downloadFileDto=null}, startPage=35, endPage=39, ext={EN=ArticleExt(id=1242138624850994100, articleId=1242138620526670147, tenantId=1146029695717560320, journalId=1146031591421210625, language=EN, title=South China Seabasin opening: Lithospheric rifting and interactionwith surroundingsubduction zones, columnId=1242138616252670854, journalTitle=Science & Technology Review, columnName=Exclusive：Exploring the deep sea in the South China Sea, runingTitle=null, highlight=null, articleAbstract=The South China Sea (SCS) is the largest marginal sea in the western Pacific Ocean. Significant breakthroughs have been made in the SCS researches, especially through the South China Sea Deep Initiative and International Ocean Discovery Program (IODP). One of the surprising discoveries is that the expected mantle serpentinites at the IODP drill sites are not found at the northern SCS continental margin; instead, the magma is found to erupt rapidly, indicating the significant magmatism at the SCS soon after the continental rifting and probably due to the strong influence of surrounding subduction zones. Thus, the SCS might be regarded as a new type of rift basin of "plate-edge rifting", different from the classic Atlantic type of "intra-plate rifting". It is also suggested that the subduction-induced mantle upwelling is likely to play an important role in the magmatism of the SCS., authors=LIN Jian^1,2,3,4, SUN Zhen^1,3,5, LI Jiabiao⁶, ZHOU Zhiyuan^1,3,5, ZHANG Fan^1,3,5, LUO Yiming^1,3,4, authorsList=LIN Jian, SUN Zhen, LI Jiabiao, ZHOU Zhiyuan, ZHANG Fan, LUO Yiming, authorCompany=1. Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;
2. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA;
3. Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou), Guangzhou 511458, China;
4. Department of Ocean Science and Engineering, Southern University of Science and Technology of China, Shenzhen 518055, China;
5. Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China;
6. Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China, correspAuthors=null, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=FBYc0TfDg9F32jEmywXGGQ==, pdfFileSize=3311476, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1242138623647228843, articleId=1242138620526670147, tenantId=1146029695717560320, journalId=1146031591421210625, language=CN, title=南海成因：岩石圈破裂与俯冲带相互作用新认识, columnId=1242138615086654327, journalTitle=科技导报, columnName=专题：南海深海探索, runingTitle=null, highlight=null, articleAbstract=南海深部计划与国际大洋钻探航次取得了一系列创新进展与重大突破：1）发现南海陆缘岩石圈减薄之初未出现地幔蛇纹岩出露，且岩浆迅速出现；2）新提出南海不是“小大西洋”，而是“板缘张裂”盆地，与经典的大西洋型“板内张裂”陆缘模式不同；3）揭示南海受到俯冲带的强烈控制，提出俯冲诱发地幔上涌并影响南海岩浆活动。, authors=林间^1,2,3,4, 孙珍^1,3,5, 李家彪⁶, 周志远^1,3,5, 张帆^1,3,5, 罗怡鸣^1,3,4, authorsList=林间, 孙珍, 李家彪, 周志远, 张帆, 罗怡鸣, authorCompany=1. 中国科学院南海海洋研究所边缘海与大洋地质重点实验室, 广州 510301;
2. 美国伍兹霍尔海洋研究所地质与地球物理系, 马萨诸塞州伍兹霍尔 02543;
3. 南方海洋科学与工程广东省实验室(广州), 广州 511458;
4. 南方科技大学海洋科学与工程系, 深圳 518055;
5. 中国科学院南海生态环境工程创新研究院, 广州 510301;
6. 自然资源部第二海洋研究所, 杭州 310012, correspAuthors=null, authorNote=林间,特聘研究员,研究方向为海洋地球物理,电子信箱:jianlin@scsio.ac.cn, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=Y+n1lb9+90AT96Tgh2sIwQ==, pdfFileSize=3311476, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=南方海洋科学与工程广东省实验室（广州）人才团队引进重大专项（GML2019ZD0205）；国家自然科学基金项目（41890813，91628301，41706056，41976066，41976064，U1606401）；中国科学院项目（Y4SL021001，QYZDY-SSW-DQC005，133244KYSB20180029）)}, authors=null, keywords=[Keyword(id=1242138623173272483, tenantId=1146029695717560320, journalId=1146031591421210625, articleId=1242138620526670147, language=CN, orderNo=1, keyword=南海), Keyword(id=1242138623282327884, tenantId=1146029695717560320, journalId=1146031591421210625, 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