THE EFFECTS OF PHOSPHATIZATION ON THE REY OF CO-RICH FE-MN CRUSTS

REN Jiangbo; HE Gaowen; YAO Huiqiang; DENG Xiguang; ZHU Kechao; YANG Shengxiong

doi:10.16562/j.cnki.0256-1492.2017.02.004

Marine Geology & Quaternary Geology > 2017 > 37(2): 33-43. > DOI: 10.16562/j.cnki.0256-1492.2017.02.004

REN Jiangbo, HE Gaowen, YAO Huiqiang, DENG Xiguang, ZHU Kechao, YANG Shengxiong. THE EFFECTS OF PHOSPHATIZATION ON THE REY OF CO-RICH FE-MN CRUSTS[J]. Marine Geology & Quaternary Geology, 2017, 37(2): 33-43. DOI: 10.16562/j.cnki.0256-1492.2017.02.004

Citation:

PDF (2752 KB)

THE EFFECTS OF PHOSPHATIZATION ON THE REY OF CO-RICH FE-MN CRUSTS

Key Laboratory of Marine Mineral Resources, MLR, Guangzhou Marine Geological Survey, Guangzhou 510075, China

More Information

Received Date: November 24, 2015
Revised Date: May 10, 2016

Graphical Abstract

Abstract

Abstract

Rare earth elements and yttrium (REY) are extremely coherent in the nature. The relative abundances of them can be used to deduce their sources or subsequent geological processes. Major elements and REY of the Co-rich Fe-Mn Crusts from Marcus-Wake Seamounts and Mid-Pacific seamounts are analyzed by XRF and ICP-MS. Combined with previous studies, REY characteristic of phosphatized and non-phosphatized Fe-Mn Crusts are emphasized respectively. Fe-Mn Crusts with low P have low ΣREY and notably positive Ce anomaly, as well as negative yttrium anomaly, after normalized by the North American shale composite(NASC). While Fe-Mn Crusts with high P have relatively high ΣREY, positive Ce anomaly and notably positive yttrium anomaly normalized by NASC. There must exist REY-rich phosphate components in the phosphatized Co-rich Fe-Mn Crusts, which are especially rich in yttrium. The issue of phosphatized crusts could be regarded as a mixed model of phosphate components and Fe-Mn crust components. Mixed model simulating result indicates that REY-rich phosphate components in Fe-Mn Crusts have the same REY pattern as seamount phosphate rock, but the content could be more than 10 times over that of seamount phosphate rock. Besides REY³⁺ and Ca²⁺, other alkali-earth metal ions can also be bound to PO₄^3- in water column, and there are numerous calcareous sediments in ocean, PO₄^3- can replace CO₃^2- in carbonate sediments to form REY-poor phosphate. However, the growth of the Fe-Mn Crust is so slow that REY has a better environment to compete with Ca at the time of PO₄^3- input, forming dissemination REY-rich phosphate. Although PO₄^3- is still mainly bound with Ca²⁺ in REY-rich phosphate, ΣREY/Ca ratio increases remarkably. This REY enrichment model may be a common geological process in non-calcium sediments in deep sea.
- REY-rich phosphates,
- Co-rich Fe-Mn crusts,
- phosphatization,
- rare earth element,
- Western Pacific Ocean

FullText(HTML)

References (50)

References

[1]	Mcmurtry G M, Vonderhaar D L, Eisenhauer A, et al. Cenozoic accumulation history of a Pacific ferromanganese crust[J]. Earth and Planetary Science Letters, 1994, 125(1-4): 105-118. doi: 10.1016/0012-821X(94)90209-7
[2]	Hein J R, Schwab W C, Davis A. Cobalt- and platinum-rich ferromanganese crusts and associated substrate rocks from the Marshall Islands[J]. Marine Geology, 1988, 78(3-4): 255-283. doi: 10.1016/0025-3227(88)90113-2
[3]	Halbach P, Hebisch U, Scherhag C. Geochemical variations of ferromanganese nodules and crusts from different provinces of the Pacific Ocean and their genetic control[J]. Chemical Geology, 1981, 34(1-2): 3-17. doi: 10.1016/0009-2541(81)90067-X
[4]	Halbach P, Segl M, Puteanus D, et al. Co-fluxes and growth-rates in ferromanganese deposits from Central Pacific seamount areas[J]. Nature, 1983, 304(5928): 716-719. doi: 10.1038/304716a0
[5]	Bolton B R, Ostwald J, Monzier M. Precious metals in ferromanganese crusts from the southwest Pacific[J]. Nature, 1986, 320(6062): 518-520. doi: 10.1038/320518a0
[6]	刘永刚, 何高文, 姚会强, 等.世界海底富钴结壳资源分布特征[J].矿床地质, 2013, 32(6): 1275-1284. doi: 10.3969/j.issn.0258-7106.2013.06.013 LIU Yonggang, HE Gaowen, YAO Huiqiang, et al. Global distribution characteristics of seafloor cobalt-rich encrustation resources[J]. Mineral Deposits, 2013, 32(6): 1275-1284. doi: 10.3969/j.issn.0258-7106.2013.06.013
[7]	潘家华, 刘淑琴.西太平洋富钴结壳的分布、组分及元素地球化学[J].地球学报, 1999, 20(1): 47-54. doi: 10.3321/j.issn:1006-3021.1999.01.007 PAN jiahua, LIU Shuqin. Distribution, composition and element geochemistry of Co-rich crusts in the Western Pacific[J]. Acta Geoscientia Sinica, 1999, 20(1): 47-54. doi: 10.3321/j.issn:1006-3021.1999.01.007
[8]	Koschinsky A, Hein J R. Uptake of elements from seawater by ferromanganese crusts: Solid-phase associations and seawater speciation[J]. Marine Geology, 2003, 198(3-4): 331-351. doi: 10.1016/S0025-3227(03)00122-1
[9]	Bau M, Koschinsky A. Oxidative scavenging of cerium on hydrous Fe oxide: Evidence from the distribution of rare earth elements and yttrium between Fe oxides and Mn oxides in hydrogenetic ferromanganese crusts[J]. Geochemical Journal, 2009, 43(1): 37-47. doi: 10.2343/geochemj.1.0005
[10]	Jiang X J, Lin X H, Yao D, et al. Enrichment mechanisms of rare earth elements in marine hydrogenic ferromanganese crusts[J]. Science China-Earth Sciences, 2011, 54(2): 197-203. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-ed201102004
[11]	任向文, 石学法, 朱爱美, 等.麦哲伦海山群MK海山富钴结壳稀土元素的赋存相态[J].吉林大学学报:地球科学版, 2011, 41(3): 707-714. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201103012 REN Xiangwen, SHI Xuefa, ZHU Aimei, et al. Existing phase of rare earth elements in Co-rich Fe-Mn crusts from seamount MK of Magellan Seamount Cluster[J]. Journal of Jilin University(Earth Science Edition), 2011, 41(3): 707-714. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201103012
[12]	Baturin G N, Yushina I G. Rare earth elements in phosphate-ferromanganese crusts on Pacific seamounts[J]. Lithology and Mineral Resources, 2007, 42(2): 101-117. doi: 10.1134/S0024490207020010
[13]	崔迎春, 石学法, 刘季花, 等.磷酸盐化作用对富钴结壳元素相关性的影响[J].地质科技情报, 2008, 27(3): 61-67. doi: 10.3969/j.issn.1000-7849.2008.03.009 CUI Yingchun, SHI Xuefa, LIU Jihua, et al. Effects of phosphatization on the elemental association of cobalt-rich crusts[J]. Geological Science and Technology Information. 2008, 27(3): 61-67. doi: 10.3969/j.issn.1000-7849.2008.03.009
[14]	Bau M, Koschinsky A, Dulski P, et al. Comparison of the partitioning behaviours of yttrium, rare earth elements, and titanium between hydrogenetic marine ferromanganese crusts and seawater[J]. Geochimica Et Cosmochimica Acta, 1996, 60(10): 1709-1725. doi: 10.1016/0016-7037(96)00063-4
[15]	Baturin G, Dubinchuk V, Azarnova L, et al. Apatite and associated minerals in ferromanganese crusts from the Magellan Seamounts[J]. Oceanology, 2006, 46(6): 869-874. doi: 10.1134/S0001437006060129
[16]	Jeong K S, Jung H S, Kang J K, et al. Formation of ferromanganese crusts on northwest intertropical Pacific seamounts: electron photomicrography and microprobe chemistry[J]. Marine Geology, 2000, 162(2-4): 541-559. doi: 10.1016/S0025-3227(99)00091-2
[17]	Koschinsky A, Stascheit A, Bau M, et al. Effects of phosphatization on the geochemical and mineralogical composition of marine ferromanganese crusts[J]. Geochimica et Cosmochimica Acta, 1997, 61(19): 4079-4094. doi: 10.1016/S0016-7037(97)00231-7
[18]	Hein J R, Yeh H W, Gunn S H, et al. Two major Cenozoic episodes of phosphogenes is records in equatorial Pacific Seamount deposits[J]. Paleoceanography, 1993, 8: 23-29. doi: 10.1029/92PA02527
[19]	武光海, 周怀阳, 凌洪飞, 等.富钴结壳中的磷酸盐岩及其古环境指示意义[J].矿物学报, 2005, 25(1): 39-44. doi: 10.3321/j.issn:1000-4734.2005.01.007 WU Guanghai, ZHOU Huaiyang, LING Hongfei, et al.Phosphorites in Co-rich crust and their palae ooceanorgaphic singificance[J]. Acta Mineralogica Sinica, 2005, 25(1): 39-44. doi: 10.3321/j.issn:1000-4734.2005.01.007
[20]	汪在聪, 李胜荣, 刘鑫, 等.中太平洋WX海山富钴结壳磷酸盐矿物学研究及成因类型分析[J].岩石矿物学杂志, 2007, 26(5): 441-448. doi: 10.3969/j.issn.1000-6524.2007.05.007 WANG Zaicong, LI Shengrong, LIU Xin. A mineralogical study and genetic analysis of phosphate in Co-rich crusts from the Central Pacific WX seamount [J]. Acta Petrologica et Mineralogica, 2007, 26(5): 441-448. doi: 10.3969/j.issn.1000-6524.2007.05.007
[21]	潘家华, 刘淑琴, 杨忆, 等.太平洋海山磷酸盐的锶同位素成分及形成年代[J].矿床地质, 2002, 21(4):350-355. doi: 10.3969/j.issn.0258-7106.2002.04.005 PAN Jiahua, LIU Shuqin, YANG Yi, et al., Sr isotopic compositions and age dating of marine phosphates from Paciific Seamounts[J]. Mineral Deposits, 2002, 21(4):350-355. doi: 10.3969/j.issn.0258-7106.2002.04.005
[22]	潘家华, 刘淑琴, 罗照华, 等.太平洋海山磷酸盐的产状、特征及成因意义[J].矿床地质, 2007, 26(2): 195-203. doi: 10.3969/j.issn.0258-7106.2007.02.006 PAN Jiahua, LIU Shuqin, LUO Zhaohua, et al. Modes of occurrence and characteristics of phosphorates on Pacific Guyots and their genetic significance[J]. Mineral Deposits, 2007, 26(2): 195-203. doi: 10.3969/j.issn.0258-7106.2007.02.006
[23]	潘家华, 刘淑琴, 杨忆, 等.西太平洋海山磷酸盐的常量微量和稀土元素地球化学研究[J].地质论评, 2002, 48(5): 534-541 doi: 10.3321/j.issn:0371-5736.2002.05.012 PAN Jiahua, LIU Shuqin, YANG Yi, et al. Research on geochemical characteristics of major, trace and rare-earth elements in phosphates from the West Pacific seamounts[J]. Geological Review, 2002, 48(5): 534-541. doi: 10.3321/j.issn:0371-5736.2002.05.012
[24]	潘家华, 刘淑琴, DeCarlo E.大洋磷酸盐化作用对富钴结壳元素富集的影响[J].地球学报, 2002, 23(5): 403-407. doi: 10.3321/j.issn:1006-3021.2002.05.003 PAN Jiahua, LIU Shuqin, DeCarlo E. The effects of marine phospharization on element concentration of cobalt rich crust[J]. Acta Geoscientia Sinica, 2002, 23(5): 403-407. doi: 10.3321/j.issn:1006-3021.2002.05.003
[25]	Duliu O G, Alexe V, Moutte J, et al. Major and trace element distributions in manganese nodules and micronodules as well as abyssal clay from the Clarion-Clipperton abyssal plain, Northeast Pacific[J]. Geo-Marine Letters, 2009, 29(2): 71-83. doi: 10.1007/s00367-008-0123-5
[26]	王吉中.磷酸盐化对中太平洋海山富钴结壳物质组分的影响[D].北京: 中国地质大学, 2005. http://cdmd.cnki.com.cn/article/cdmd-11415-2005102558.htm WANG Jizhong. Effects of phosphatization on composition of Co-rich crusts crusts on Central Pacific seamounts[D]. China University of Geosciences: Beijing, 2005. http://cdmd.cnki.com.cn/article/cdmd-11415-2005102558.htm
[27]	Pan J H, De Carlo E H, Yang Y, et al. Effect of phosphatization on element concentration of cobalt-rich ferromanganese crusts[J]. Acta Geologica Sinica-English Edition, 2005, 79(3): 349-355. doi: 10.1111/j.1755-6724.2005.tb00900.x
[28]	Kon Y, Hoshino M, Sanematsu K, et al. Geochemical characteristics of apatite in heavy REE-rich deep-sea mud from Minami-Torishima area, Southeastern Japan[J]. Resource Geology, 2014, 64: 47-57. doi: 10.1111/rge.12026
[29]	任江波, 姚会强, 朱克超, 等.稀土元素和钇在东太平洋CC区深海泥中的富集特征及机制[J].地学前缘, 2015, 22(4): 200-211. http://www.cqvip.com/QK/98600X/201504/665043589.html REN Jiangbo, YAO Huiqiang, ZHU Kechao, et al. Enrichment mechanisms of rare earth elements and yttrium in deep-sea mud of Clarion-Clipperton Region[J]. Earth Science Frontiers(China University of Geosciences(Beijing)), 2015, 22(4): 200-211. http://www.cqvip.com/QK/98600X/201504/665043589.html
[30]	Alibo D S, Nozaki Y. Rare earth elements in seawater: Particle association, shale-normalization, and Ce oxidation[J]. Geochimica Et Cosmochimica Acta, 1999, 63(3-4): 363-372. doi: 10.1016/S0016-7037(98)00279-8
[31]	潘家华, Carlo E D, 刘淑琴, 等.西太平洋富钴结壳生长与富集特征[J].地质学报, 2005, 79(1): 124-132. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200501014 PAN Jiahua, Carlo E D, LIU Shuqin, et al. Growth and enrichment characteristics of Co-rich crusts in the Western Pacific[J].Acta Geologica Sinica, 2005, 79(1): 124-132. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200501014
[32]	潘家华, 张静, 刘淑琴, 等.西北太平洋富钴结壳的钙质超微化石地层学研究及意义[J].地球学报, 2007, 28(5):411-417. doi: 10.3321/j.issn:1006-3021.2007.05.001 PAN Jiahua, ZHANG Jing, LIU Shuqin, et al.Calcareous nannofossil biostratigraphy of Co-rich crusts from Northwestern Pacific and its significance[J]. Acta Geoscientica Sinica, 2007, 28(5):411-417. doi: 10.3321/j.issn:1006-3021.2007.05.001
[33]	何高文, 孙晓明, 杨胜雄, 等.太平洋多金属结核和富钴结壳稀土元素地球化学对比及其地质意义[J].中国地质, 2011, 38(2): 462-472. doi: 10.3969/j.issn.1000-3657.2011.02.020 HE Gaowen, SUN Xiaoming, YANG Shengxiong, et al. A comparison of REE geochemistry between polymetallic nodules and cobaltrich crusts in the Pacific Ocean[J]. Geology in China, 2011, 38(2): 462-472. doi: 10.3969/j.issn.1000-3657.2011.02.020
[34]	Hein J R, Conrad T, Frank M, et al. Copper-nickel-rich, amalgamated ferromanganese crust-nodule deposits from Shatsky Rise, NW Pacific[J]. Geochemistry, Geophysics, Geosystems, 2012, 13(10): 1-23.
[35]	任江波, 姚会强, 朱克超, 等.西太平洋海山区富钴结壳的稀土元素特征及其意义[J].地质论评, 2013, 59(S): 1248-1249. http://d.old.wanfangdata.com.cn/Conference/8101661 REN Jiangbo, YAO Huiqiang, ZHU Kechao, et al. The characteristics of rare erath elements and its significance of Co-rich crusts from Western Pacific seamounts[J]. Geological Review, 2013, 59(S): 1248-1249. http://d.old.wanfangdata.com.cn/Conference/8101661
[36]	Klemm V, Levasseur S, Frank M, et al. Osmium isotope stratigraphy of a marine ferromanganese crust[J]. Earth and Planetary Science Letters, 2005, 238(1-2): 42-48. doi: 10.1016/j.epsl.2005.07.016
[37]	潘家华, 刘淑琴, 钟石兰.西太平洋富钴结壳形成年代的探讨[J].地质论评, 2002, 48(5), 463-467. doi: 10.3321/j.issn:0371-5736.2002.05.003 PAN Jiahua, LIU Shuqin, ZHONG Shilan, et al. Rasearch on the age of cobalt-rich crusts in Western Pacific[J]. Geological Review, 2002, 48(5): 463-467. doi: 10.3321/j.issn:0371-5736.2002.05.003
[38]	何高文, 邓希光, 杨胜雄.中印度洋海盆多金属结核地质特征[J].海洋地质与第四纪地质, 2011, 31(2): 21-30. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201102003 HE Gaowen, DENG Xiguang, YANG Shengxiong. Geological characteristics of polymetallic nodules ain the central Indian Ocean [J]. Marine Geogogy and Quaternary Geology, 2011, 31(2): 21-30. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201102003
[39]	刘新波.太平洋中部多金属结核矿物地球化学研究[D].青岛: 中国海洋大学, 2005. http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=Y829277 LIU Xinbo. Study on mineralogy and geochemitry of polymetallic nodules from the Central and Eastern Pacific Ocean[D].Ocean University of China, 2005. http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=Y829277
[40]	Lécuyera C, Reynardb B, Grandjean P. Rare earth element evolution of Phanerozoic seawater recorded in biogenic apatites[J]. Chemical Geology, 2004, 204(1-2): 63-102. doi: 10.1016/j.chemgeo.2003.11.003
[41]	Shields G A, Webb G E. Has the REE composition of seawater changed over geological time[J]. Chemical Geology, 2004, 204(1-2): 103-107. doi: 10.1016/j.chemgeo.2003.09.010
[42]	Gromet L P, Dymer R F, Haskin L A, et al. The "north American shale composition": Its complication, major and trace element characteristics[J]. Geochimica et Cosmochimica Acta, 1984, 48: 2469-2482. doi: 10.1016/0016-7037(84)90298-9
[43]	Toyoda K, Tokonami M. Diffusion of rare-earth elements in fish teeth from deep-sea sediments[J]. Nature, 1990, 345: 607-609. doi: 10.1038/345607a0
[44]	Paytan A, McLaughlin K. The oceanic phosphorus cycle[J]. Chemical Reviews, 2007, 107(2): 563-576. doi: 10.1021/cr0503613
[45]	Elderfield H, Greaves M J. The rare earth elements in seawater[J]. Nature, 1982, 296: 214-219. doi: 10.1038/296214a0
[46]	Byrne R H, Kim K H. Rare earth precipitation and coprecipitation behavior: The imiting role of PO₄^3-: On dissolved rare earth concentrations in seawater[J]. Geochemica et Cosmochemica Acta, 1993, 57: 519-526. doi: 10.1016/0016-7037(93)90364-3
[47]	Jones E J W, BouDagher-Fadel M K, Thirlwall M F. An investigation of seamount phosphorites in the Eastern Equatorial Atlantic[J]. Marine Geology, 2002, 183(1-4): 143-162. doi: 10.1016/S0025-3227(01)00254-7
[48]	潘家华, 刘淑琴, 杨忆, 等.太平洋水下海山磷酸盐的成因及形成环境[J].地球学报, 2004, 25(4):453-458. doi: 10.3321/j.issn:1006-3021.2004.04.011 PAN Jia-hua, LIU Shuqin, YANG Yi, et al., The origin and formation environment of phosphates on submarine guyots of the Pacific Ocean[J]. Acta Geoscientica Sinica, 2004, 25(4):453-458. doi: 10.3321/j.issn:1006-3021.2004.04.011
[49]	Toyoda K, Nakamura Y, Masuda A. Rare earth elements of Pacific pelagic sediments[J]. Geochimica et Cosmochimica Acta, 1990, 54(4): 1093-1103. doi: 10.1016/0016-7037(90)90441-M
[50]	Liu J, Shi X, Chen L, et al. REEs and εNd of clay fractions in sediments from the eastern Pacific Ocean - Evidences for clay sources[J]. Science China-Earth Sciences, 2004, 33(6): 552-561. http://www.cnki.com.cn/Article/CJFDTotal-JDXG200505009.htm

[1]	KONG Xianghuai, LU Kai, XU Xiaoda, YANG Huiliang, ZHANG Yong, SHANG Luning. A study on the characteristic and its cause of topography and geomorphology of the South Yellow Sea[J]. Marine Geology & Quaternary Geology, 2022, 42(6): 21-31. DOI: 10.16562/j.cnki.0256-1492.2022072903
[2]	QIN Yachao, GAO Fei, SU Dapeng, ZHU Xiaoqing, XIE Liujuan. Late spring thermocline and chemoclines in the area off the Rizhao–Lianyungang coast, western South Yellow Sea[J]. Marine Geology & Quaternary Geology, 2021, 41(3): 22-32. DOI: 10.16562/j.cnki.0256-1492.2020080301
[3]	ZHU Yingtao, FENG Xiuli, ZHU Longhai, HU Rijun, JIANG Shenghui. Seasonal distribution of suspended sediments in the water northeast to Shandong Peninsula and its controlling factors[J]. Marine Geology & Quaternary Geology, 2021, 41(2): 30-42. DOI: 10.16562/j.cnki.0256-1492.2020032201
[4]	LI Wenjian, WANG Zhenyan, HUANG Haijun. Grain size distribution pattern and influencing factors of suspended matters in the Southern Yellow Sea during summer season[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 49-60. DOI: 10.16562/j.cnki.0256-1492.2020011002
[5]	PANG Xiaolei, DING Xuan. VARIATION IN SURFACE AND THERMOCLINE TEMPERATURE OF THE EASTERN TIMOR SEA FOR THE LAST 30 KA AND ITS PALEOCEANOGRAPHIC IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2015, 35(2): 117-124. DOI: 10.3724/SP.J.1140.2015.02117
[6]	XIAO Hehui, WANG Houjie, BI Naishuang, WU Xiao, WANG Aimei, ZHANG Yong. SEASONAL VARIATION OF SUSPENDED SEDIMENT IN THE BOHAI AND YELLOW SEA AND THE PATHWAY OF SEDIMENT TRANSPORT[J]. Marine Geology & Quaternary Geology, 2015, 35(2): 11-21. DOI: 10.3724/SP.J.1140.2015.02011
[7]	LI Jianchao, QIAO Lulu, LI Guangxue, LIU Yong, MA Yanyan, LIU Ling. DISTRIBUTION OF WINTER SUSPENDED PARTICULATE MATTERS IN THE SOUTH YELLOW SEA BASED ON LISST DATA[J]. Marine Geology & Quaternary Geology, 2013, 33(5): 13-25. DOI: 10.3724/SP.J.1140.2013.05013
[8]	CHEN Xiaohui, LI Rihui, XU Xiaoda. SHALLOW SEISMIC RECORDS AND LATE PLEISTOCENE STRATIGRAPHY OF THE NORTH YELLOW SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(3): 17-22. DOI: 10.3724/SP.J.1140.2011.03017
[9]	ZHANG Haiqi, CHEN Jianwen, LI Gang, WU Zhiqiang, ZHANG Yinguo. DISCOVERY FROM SEISMIC SURVEY IN LAOSHAN UPLIFT OF THE SOUTH YELLOW SEA AND THE SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2009, 29(3): 107-113. DOI: 10.3724/SP.J.1140.2009.03107
[10]	SONG Zhao-jun, HUANG Hai-jun, DU Ting-qin, LIU Fang, NI Jin-long. SUSPENDED SEDIMENT NEAR RADIAL SAND RIDGE AREA IN THE SOUTH YELLOW SEA[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 19-25.

Cited By

Cited by

Periodical cited type(9)

1.	徐超，陈春强，邓继新，米中荣，杨滔，瞿建华，白桦，罗春树，杨鸿，洪余刚，赵星，肖勇. 伊拉克中部E油田三角洲前缘Zubair层系砂岩储层预测. 科学技术与工程. 2020(26): 10734-10739 .
2.	吴淑玉，徐华宁，刘俊，杨睿，宁伏龙. 南海神狐海域非均质性天然气水合物储层的分频反演. 海洋地质与第四纪地质. 2020(06): 106-120 . 本站查看
3.	孟大江，文鹏飞，张宝金，张如伟，李延，赵斌，沈尚峰. 天然气水合物储层反演及饱和度预测. 海洋地质前沿. 2019(11): 43-51 .
4.	Yan-long Li，Yi-zhao Wan，Qiang Chen，Jia-xin Sun，Neng-you Wu，Gao-wei Hu，Fu-long Ning，Pei-xiao Mao. Large borehole with multi-lateral branches: A novel solution for exploitation of clayey silt hydrate. China Geology. 2019(03): 333-341 .
5.	龚跃华，杨胜雄，王宏斌，梁金强，梁劲. 琼东南盆地天然气水合物成矿远景. 吉林大学学报(地球科学版). 2018(04): 1030-1042 .
6.	闫华，王晓燕，寇枫，卢雄. 基于地震波阻抗反演的薄储层定量预测技术. 非常规油气. 2018(04): 1-7 .
7.	孟大江，文鹏飞，张旭东. AVO反演在琼东南海域天然气水合物识别中的应用. 海洋地质前沿. 2018(07): 46-55 .
8.	徐云霞，文鹏飞，张如伟，张宝金，薛花. 无井波阻抗反演在西沙水合物研究中的应用. CT理论与应用研究. 2017(04): 425-434 .
9.	王凯，陈德元，张凯，岳航羽，张保卫，王小江. 青海木里地区陆域天然气水合物地震波阻抗特征研究. 物探与化探. 2017(06): 1105-1112 .

Other cited types(2)

Get Citation

PDF

XML

Article views (2469) PDF downloads (24) Cited by(11)

Turn off MathJax

Article Contents

Abstract

References

THE EFFECTS OF PHOSPHATIZATION ON THE REY OF CO-RICH FE-MN CRUSTS