Article(id=1242138628860752235, tenantId=1146029695717560320, journalId=1146031591421210625, issueId=1242138608648397669, articleNumber=null, orderNo=13, doi=10.3981/j.issn.1000-7857.2020.18.011, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1586880000000, receivedDateStr=2020-04-15, revisedDate=1592409600000, revisedDateStr=2020-06-18, 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=1774078526937, creator=sys-migrate, updateTime=1774078526937, 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=68, endPage=74, ext={EN=ArticleExt(id=1242138633898107858, articleId=1242138628860752235, tenantId=1146029695717560320, journalId=1146031591421210625, language=EN, title=The evolution of the carbonate platforms in the South China Sea, columnId=1242138616252670854, journalTitle=Science & Technology Review, columnName=Exclusive：Exploring the deep sea in the South China Sea, runingTitle=null, highlight=null, articleAbstract=The evolution of the Cenozoic reefs-carbonate platform is considered a part of the South China Sea opening, and plays an important role in the deepwater hydrocarbon reservoirs, the global carbon circulation, and the South China Sea tectonic history. The platforms were formed during the early Miocene, and flourished during the early Middle Miocene. However, they became drowned since the Middle Miocene, and many platforms disappeared during the Quaternary. It is found that the carbonate platform of the South China Sea sees a developmental pattern from south to north and from east to west. The highest accumulation rate of the platform was reached during the Middle Miocene. The control of the platform life history is very complex. But the most important four factors are the tectonic activities, the changes in the relative sea level, the changes in the input of the terrestrial detrital materials, and the changes in the paleo-ocean environment, and they are considered to control the development and the death of the reefs-carbonate platform., authors=WU Shiguo1 , YU Kefu2 , LI Xuelin1 , ZHANG Hanyu1 , CHEN Wanli1 , authorsList=WU Shiguo, YU Kefu, LI Xuelin, ZHANG Hanyu, CHEN Wanli, authorCompany=1. Laboratory of Marine Geophysics and Georesources, Institute of Deep-sea Science and Engineering, CAS, Sanya 572000, China;1 , 余克服2 , 李学林1 , 张汉羽1 , 陈万利1 , authorsList=吴时国, 余克服, 李学林, 张汉羽, 陈万利, authorCompany=1. 中国科学院深海科学与工程研究所, 海南省海底资源与探测技术重点实验室, 三亚 572000;
科技导报
| 专题：南海深海探索 2020, 38(18): 68-74
南海生物礁碳酸盐台地演化
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吴时国1 , 余克服2 , 李学林1 , 张汉羽1 , 陈万利1
作者信息
1. 中国科学院深海科学与工程研究所, 海南省海底资源与探测技术重点实验室, 三亚 572000;
The evolution of the carbonate platforms in the South China Sea
Affiliations
出版时间: 2020-09-28
doi: 10.3981/j.issn.1000-7857.2020.18.011
文章导航
南海碳酸盐台地分布自早中新世开始发育，至中中新世达到鼎盛，再到晚中新世大量台地被淹没而逐渐消亡。从分布看，南海碳酸盐台地具有南早北晚、东早西晚的发育规律；从堆积速率看，中中新统速率最大。控制这些台地的诞生、发育演化和消亡的因素十分复杂，可能包括构造活动、相对海平面的变化、陆源碎屑物质输入变化、古海洋环境变化。
碳酸盐台地
/
生物礁
/
海平面
/
陆源碎屑
/
南海
The evolution of the Cenozoic reefs-carbonate platform is considered a part of the South China Sea opening, and plays an important role in the deepwater hydrocarbon reservoirs, the global carbon circulation, and the South China Sea tectonic history. The platforms were formed during the early Miocene, and flourished during the early Middle Miocene. However, they became drowned since the Middle Miocene, and many platforms disappeared during the Quaternary. It is found that the carbonate platform of the South China Sea sees a developmental pattern from south to north and from east to west. The highest accumulation rate of the platform was reached during the Middle Miocene. The control of the platform life history is very complex. But the most important four factors are the tectonic activities, the changes in the relative sea level, the changes in the input of the terrestrial detrital materials, and the changes in the paleo-ocean environment, and they are considered to control the development and the death of the reefs-carbonate platform.
carbonate platform
/
coral reef
/
sea level
/
terrigenous clast
/
South China Sea
吴时国, 余克服, 李学林, 张汉羽, 陈万利.
南海生物礁碳酸盐台地演化.
科技导报,
2020
, 38
(18)
: 68
-74
.
DOI: 10.3981/j.issn.1000-7857.2020.18.011
WU Shiguo, YU Kefu, LI Xuelin, ZHANG Hanyu, CHEN Wanli.
The evolution of the carbonate platforms in the South China Sea[J].
Science & Technology Review ,
2020
, 38
(18)
: 68
-74
.
DOI: 10.3981/j.issn.1000-7857.2020.18.011
2020年第38卷第18期
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文章信息
doi: 10.3981/j.issn.1000-7857.2020.18.011
接收时间：2020-04-15
首发时间：2020-11-04
出版时间：2020-09-28
收稿日期：2020-04-15
修回日期：2020-06-18
https://castjournals.cast.org.cn/joweb/kjdb/CN/10.3981/j.issn.1000-7857.2020.18.011
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2种不同金属材料的力学参数
科 属数 种数 占总种数比例 属 种数 占总种数比例 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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