Journal of Tropical Oceanography ›› 2020, Vol. 39 ›› Issue (6): 18-29.doi: 10.11978/YG2020002CSTR: 32234.14.YG2020002
• Review • Previous Articles Next Articles
International collaboration of ocean exploration in the South China Sea enhanced by International Ocean Discovery Program Expeditions 367/368/368x
SUN Zhen1,2,3(
), LIN Jian1,2,3, WANG Pinxian4, JIAN Zhimin4, LI ChunFeng5
- 1. CAS Key Laboratory of Ocean and Marginal Sea Geology (South China Sea Institute of Oceanology), Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China
2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
3. China-Pakistan Joint Research Center on Earth Sciences, Islamabad 45320, Pakistan
4. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
5. Department of Marine Sciences, Zhejiang University, Zhoushan 316021, China
-
Received:2020-05-25Revised:2020-06-24Online:2020-10-10Published:2020-12-03 -
Contact:SUN Zhen E-mail:zhensun@scsio.ac.cn -
Supported by:Guangdong NSF research team project(2017A030312002);K.C. Wong Education Foundation(GJTD-2018-13);Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0104);Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0205);Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(2019BT02H594)
CLC Number:
- P738
Cite this article
SUN Zhen, LIN Jian, WANG Pinxian, JIAN Zhimin, LI ChunFeng. International collaboration of ocean exploration in the South China Sea enhanced by International Ocean Discovery Program Expeditions 367/368/368x[J].Journal of Tropical Oceanography, 2020, 39(6): 18-29.
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Fig. 1
The main structural framework of the South China Sea and the distribution of ODP/IODP drill sites. The red square in the left panel is the area displayed in the right panel. The black lines in the right panel indicate the sections of the seismic profiles displayed in Fig. 3. Magnetic anomaly lineations are after Briais et al (1993)"
Fig. 1
Tab. 1
Review history of IODP878 proposal"
| 时间 | 建议书提交情况 | 评审情况 | |
|---|---|---|---|
| 2013年10月 | 提交初始建议书838-pre | 2013年11月, 科学与站位评估委员会(SEP)评审, 鼓励提交完整建议 | |
| 2014年4月 | 提交完整建议书838-full | 2014年5月, 科学与站位评估委员会(SEP)评审, 并建议修改 | |
| 2014年10月 | 提交修改后建议书838-full2 | 2014年11月, SEP评审, 建议书被拒绝, 并鼓励修改后重新提交 | |
| 2015年4月 | 通过与中海油合作, 补充采集新地震资料, 提交修改后建议书, 重新编号878-CPP | 2015年5月, SEP通过评审, 并建议提交环境保护与安全委员会(EPSP)进行站位安全和环境保护评估 | |
| 2015年9月 | 提交航次计划和站位建议至EPSP | EPSP通过部分站位评估, 但建议需补充更多备选站位后再次评估 | |
| 2016年3月 | 增加备选站位设计, 再次提交全部站位资料至EPSP | 2016年7月, EPSP对878-CPP建议书和站位资料进行再次评估, 通过钻探建议和方案, 送JRSF, 正式进入航次安排; | |
| 2016年10月 | 确定为IODP367/368航次, 执行时间2017年2—6月 | ||
Tab. 1
Fig. 2
The stratigraphic column of all drill sites of IODP expeditions 367, 368, and 368X (Sun et al, 2018a; Jian et al, 2018a)"
Fig. 2
Tab. 2
Coring information at all the drill sites of IODP 367/368/368X"
| 钻孔 | 经度 | 纬度 | 水深/m | 进尺/m | 取芯/m | 取芯率/% | 位置及科学目标 |
|---|---|---|---|---|---|---|---|
| U1499A | 115°51'35"E | 18°24'34"N | 3760.2 | 659.2 | 417.05 | 63.27 | 洋陆过渡带, 检验下地壳或地幔剥露 |
| U1499B | 115°51'36"E | 18°24'34"N | 3758.1 | 1081.8 | 150.64 | 35.3 | |
| U1500A | 116°13'11"E | 18°18'17"N | 3801.7 | 854.6 | 93.55 | 28.37 | 早期洋壳, 检验是否下地壳或地幔剥露 |
| U1500B | 116°13'12"E | 18°18'16"N | 3801.6 | 1529 | 278.79 | 40.82 | |
| U1501C | 115°45'57"E | 18°53'06"N | 2845.81 | 461.9 | 444.77 | 96.29 | 远端带, 揭示完整张破裂层序 |
| U1501D | 115°45'56"E | 18°53'06"N | 2845.82 | 644.3 | 78.77 | 37.37 | |
| U1502A | 116°13'50"E | 18°27'52"N | 3763.72 | 758.2 | 176.81 | 46.14 | 洋陆过渡带, 检验是否有下地壳或地幔剥露 |
| U1502B | 116°13'50"E | 18°27'53"N | 3763.58 | 920.8 | 131.57 | 68.14 | |
| U1503A | 116°18'51"E | 18°8'38"N | 3867.71 | 1710.1 | 175.73 | 10.29 | 成熟洋盆, 检验洋盆发育时间和成分 |
| U1504A | 116°14'32"E | 18°50'55"N | 2816.57 | 165.5 | 52.93 | 31.98 | 外缘隆起, 检验基底组成 |
| U1504B | 116°14'36"E | 18°50'49"N | 2842.97 | 200 | 21.48 | 19.21 | |
| U1505C | 115°51'33"E | 18°55'03"N | 2917.37 | 480.2 | 480.15 | 99.99 | 远端带盆地, 检验渐新世以来环境变化 |
| U1505D | 115°51'33"E | 18°55'03"N | 2917 | 184.5 | 191.43 | 103.76 | |
| 合计 | 9650.1 | 2693.67 |
Tab. 2
Fig. 3
Seismic profiles across or projected with all the drill sites. The locations of the profiles are shown in the right panel of Fig. 1. Site name ending with P means projected site. C11r and C10r are magnetic lineations and correspond to 31-30 Ma and 29 Ma, respectively. The dotted green line is the Moho recognized on Multi-Channel seismic profile, while the dotted red line is the upper/lower crust boundary (ULB). The red arrows indicate the pull-up reflections, suggesting magmatic intrusion"
Fig. 3
Fig. 4
The basement rocks encountered at the drill sites from COT to the ocean"
Fig. 4
Fig. 5
Schematic diagram showing that magmatism of the South China Sea during rifting and spreading might be affected strongly by subduction (modified slightly after Sun et al, 2019; Shi et al, 2012). a) During late Mesozoic, the South China Sea is under subduction. Around 60-50 Ma, the ridge subducted toward Eurasia (Seton et al, 2015). The ridge subduction and slab break-away for the front block may have caused large amount of magmatism and ground uplift. b) During early Cenozoic, the South China Sea transformed into extensional margin. According to the cessation of volcanic magmatism in the northern margin around 50 Ma (Li et al, 2018), and accretionary wedge development between the southern margin and the northern Borneo at about 45 Ma (Madon et al, 2013), the slab had started to subduct toward south and caused rifting or even spreading. c) The fertile mantle stimulated by the slab break-off arrive at the seafloor and caused another stage of magmatism and ground uplift"
Fig. 5
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