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2. Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China;
3. South China Sea Institute of Oceanography, Chinese Academy of Sciences, Guangzhou 310012, China, correspAuthors=null, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=ebLqOI1zRAzFIjtolSgsLg==, pdfFileSize=2170329, 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=1242138624926491573, articleId=1242138621822706593, tenantId=1146029695717560320, journalId=1146031591421210625, language=CN, title=南海海盆演变与深部海流, columnId=1242138615086654327, journalTitle=科技导报, columnName=专题:南海深海探索, runingTitle=null, highlight=null, articleAbstract=南海在距今34 Ma之前的始新世从陆地变为海洋,古水深不断加深,至距今24 Ma之前的中新世/渐新世之交,由于T60构造运动,南海海盆整体进入深海环境。但是,自中新世以来随着吕宋岛弧向欧亚板块碰撞,南海海盆的半封闭程度在距今10.0、6.5、3.0和1.2 Ma之前加剧,导致南海深部海水只能来自巴士海峡海槛深度2600 m以浅的太平洋。此后,巴士海峡两侧的南海与太平洋深部海水交换,由于全球海平面变化,呈现冰期/间冰期模式。, authors=翦知湣1 , 田军1 , 黄维1 , 马小林2 , 万随3 , authorsList=翦知湣, 田军, 黄维, 马小林, 万随, authorCompany=1. 同济大学海洋与地球科学学院, 海洋地质国家重点实验室, 上海 200092;
2. 中国科学院地球环境研究所, 西安 710061;
3. 中国科学院南海海洋研究所, 广州 310012, correspAuthors=null, authorNote=翦知湣,教授,研究方向为海洋地质学,电子信箱:jian@tongji.edu.cn, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=5beEVbmeyqUiEEdEFwWDdg==, pdfFileSize=2170329, 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=国家自然科学基金重大研究计划项目(91428310);国家重点研发计划项目(2018YFE0202400))}, authors=[Author(id=1278619410525040728, tenantId=1146029695717560320, journalId=null, articleId=1242138621822706593, orderNo=null, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=null, email=null, emailSecond=null, emailThird=null, correspondingAuthor=null, authorType=null, ext={}, companyList=null)], 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科技导报
| 专题:南海深海探索 2020, 38(18): 52-56
南海海盆演变与深部海流
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Evolution of the South China Sea basin and the deep circulation
Affiliations
出版时间: 2020-09-28
doi: 10.3981/j.issn.1000-7857.2020.18.008
文章导航
南海在距今34 Ma之前的始新世从陆地变为海洋,古水深不断加深,至距今24 Ma之前的中新世/渐新世之交,由于T60构造运动,南海海盆整体进入深海环境。但是,自中新世以来随着吕宋岛弧向欧亚板块碰撞,南海海盆的半封闭程度在距今10.0、6.5、3.0和1.2 Ma之前加剧,导致南海深部海水只能来自巴士海峡海槛深度2600 m以浅的太平洋。此后,巴士海峡两侧的南海与太平洋深部海水交换,由于全球海平面变化,呈现冰期/间冰期模式。
深水古海洋学
/
南海
/
海盆演变
/
冰期旋回
The present-day South China Sea (SCS) was evolved from land to sea in the Eocene 34 million years ago, and its paleo-water was very deep. At the turn of the Miocene/Oligocene, 24 million years ago, due to the T60 tectonic movement, the entire SCS basin became a deep-sea environment. Since the Miocene, 10.0, 6.5 and 1.2 million years ago, along with the collision of the Luzon island arc with the Eurasian plate, the semi-closed degree of the SCS basin increased, so that the SCS deep-water could only come from the Pacific above the sill depth (~2600 m) of the Bashi Strait. After that, due to the global sea level change, the deep-water exchange between the SCS and the Pacific on both sides of the Bashi Strait displayed the glacial/interglacial mode.
deep-water paleoceanography
/
South China Sea
/
basin evolution
/
glacial cycle
翦知湣, 田军, 黄维, 马小林, 万随.
南海海盆演变与深部海流.
科技导报,
2020
, 38
(18)
: 52
-56
.
DOI: 10.3981/j.issn.1000-7857.2020.18.008
JIAN Zhimin, TIAN Jun, HUANG Wei, MA Xiaolin, WAN Sui.
Evolution of the South China Sea basin and the deep circulation[J].
Science & Technology Review ,
2020
, 38
(18)
: 52
-56
.
DOI: 10.3981/j.issn.1000-7857.2020.18.008
2020年第38卷第18期
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doi: 10.3981/j.issn.1000-7857.2020.18.008
接收时间:2020-05-11
首发时间:2020-11-04
出版时间:2020-09-28
收稿日期:2020-05-11
修回日期:2020-06-21
https://castjournals.cast.org.cn/joweb/kjdb/CN/10.3981/j.issn.1000-7857.2020.18.008
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2种不同金属材料的力学参数
科 Family 属数 Number of genus 种数 Number of species 占总种数比例 Percentage of total species (%) 属 Genus 种数 Number of species 占总种数比例 Percentage of total species (%) 鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78 小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39 多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39 红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87 小菇属 Mycena 11 5.26 光柄菇属 Pluteus 5 2.39 红菇属 Russula 17 8.13 栓菌属 Trametes 5 2.39
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