[1]Wang Zhenfeng.Important deepwater hydrocarbon reservoirs:The Central Canyon System in the Qiongdongnan Basin[J].Acta Sedimentologica Sinica,2012,30(4):646-653.[王振峰.深水重要油气储层——琼东南盆地中央峡谷体系[J].沉积学报,2012,30(4):646-653.]
[2]Zhang Daojun,Wang Yahui,Wang Zhenfeng,et al.Characteristics of sedimentary microfacies in the Central Canyon with in the deep water area,Qiongdongnan Basin[J].Acta Sedimentologica Sinica,2013,31(6):1114-1121.[张道军,王亚辉,王振峰,等.琼东南盆地深水区中央峡谷沉积微相特征[J].沉积学报,2013,31(6):1114-1121.]
[3]Zuo Qianmei,Zhang Daojun,He Weijun,et al.Provenance analysis of Huangliu Formation of the Central Danyon System in the deepwater area of the Qiongdongnan Basin[J].Acta Oceanologica Sinica,2015,37(5):63-61.[左倩媚,张道军,何卫军,等.琼东南盆地深水区中央峡谷黄流组物源特征[J].海洋学报,2015,37(5):63-61.]
[4]Wang Zhenfeng,Sun Zhipeng,Zhang Yingchao,et al.Distribution and hydrocarbon accumulation mechanism of the giant deepwater Central Canyon Gasfield in Qiongdongnan Basin,northern South China Sea[J].China Petroleum Exploration,2016,21(4):54-64.[王振峰,孙志鹏,张迎朝,等.南海北部琼东南盆地深水中央峡谷大气田分布与成藏规律[J].中国石油勘探,2016,21(4):54-64.]
[5]Su Ming,Zhang Cheng,Xie Xinong,et al.Controlling factors on the submarine canyon system:A case study of the Central Canyon System in the Qiongdongnan Basin,northern South China Sea[J].Science China:Earth Sciences,2014(8):1807-1820.[苏明,张成,解习农,等.深水峡谷体系控制因素分析——以南海北部琼东南盆地中央峡谷体系为例[J].中国科学:地球科学,2014(8):1807-1820.]
[6]Wang Yahui,Zhang Daojun,Zhao Pengxiao,et al.A new consideration on the genetic mechanism of the Central Canyon in the Qiongdongnan Basin,the northern South China Sea[J].Acta Oceanologica Sinica,2016,38(11):97-104.[王亚辉,张道军,赵鹏肖,等.南海北部琼东南盆地中央峡谷成因新认识[J].海洋学报,2016,38(11):97-104.]
[7]Li Dong,Xu Qiang,Wang Yongfeng.Provenance analysis of thePpliocene Central Canyon in Qiongdongnan Basin and its implications[J].Acta Sedimentologica Sinica,2015,33(4):659-664.[李冬,徐强,王永凤.琼东南盆地上新世中央峡谷物源分析及其意义[J].沉积学报,2015,33(4):659-664.]
[8]Huang Wei,Xie Xinong,He Yunlong,et al.Evolution and reservoir prediction of Yinggehai Formation in western Central Canyon in Qiongdongnan Basin[J].Acta Sedimentologica Sinica,2015,33(4):809-816.[黄卫,解习农,何云龙,等.琼东南盆地中央峡谷西段莺歌海组沉积演化及储层预测[J].沉积学报,2015,33(4):809-816.]
[9]Yan Y,Carter A,Palk C,et al.Understanding sedimentation in the Song Hong-Yinggehai Basin,South China Sea[J].Geochemistry Geophysics Geosystems,2011,12(6):48-58.
[10]Xiu C,Sun Z,Zhai S,et al.U-Pb ages of detrital zircons from deep-water well core in the Qiongdongnan Basin and implications for provenance[J].Ocean University of China,Qingdao,2015,In press.
[11]Liu Y S,Gao S,Hu Z C,et al.Continental and oceanic crust recycling-induced melt-peridotite interactions in the trans-north China orogen:U-Pb dating,Hf isotopes and trace elements in zircons from mantle xenoliths[J].Journal of the Geological Society,2009,51(51):537-571.
[12]Andersen T.Correction of common lead in U-Pb analyses that do not report204Pb[J].Chemical Geology,2002,192(1-2):59-79.
[13]Compston W,Williams I S,Kirschvink J L,et al.Zircon U-Pb ages for the Early Cambrian time-scale[J].Journal of the Geological Society,1992,149(2):171-184.
[14]Vermeesch P.On the visualisation of detrital age distributions[J].Chemical Geology,2012,312-313(3):190-194.
[15]Rollinson H.Using geochemical data:Evaluation,presentation,interpretation[J].Longman Scientific and Technical,USA,1994,58(392):523-523.
[16]Mclennan S M.Rare earth elements and sedimentary rocks:Influence of provenance and sedimentary processes[J].Reviews in Mineralogy,1989,21(8):169-200.
[17]Wang C,Liang X,Xie Y,et al.Provenance of Upper Miocene to Quaternary sediments in the Yinggehai-Song Hong Basin,South China Sea:Evidence from detrital zircon U-Pb ages[J].Marine Geology,2014,355(9):202-217.
[18]Zhao M,Shao L,Liang J,et al.No Red River capture since the Late Oligocene:Geochemical evidence from the northwestern South China Sea[J].Deep Sea Research Part II Topical Studies in Oceanography,2015,122:185-194.
[19]Zhong Zehong,Liu Jinghuan,Zhang Daojun,et al.Origin and sedimentary reservoir characteristics of a large submarine fan in Dongfang area,Yinggehai Basin[J].Acta Petrolei Sinica,2013,34(supplement 2):102-111.[钟泽红,刘景环,张道军,等.莺歌海盆地东方区大型海底扇成因及沉积储层特征[J].石油学报,2013,34(增刊2):102-111.]
[20]Jiang T,Cao L C,Xie X N,et al.Insights from heavy minerals and zircon U-Pb ages into the middle Miocene-Pliocene provenance evolution of the Yinggehai Basin,northwestern South China Sea[J].Sedimentary Geology,2015,327:32-42.
[21]Cao L C,Jiang T,Wang Z F,et al.Provenance of Upper Miocene sediments in the Yinggehai and Qiongdongnan Basins,northwestern South China Sea:Evidence from REE,heavy minerals and zircon U-Pb ages[J].Marine Geology,2015,361:136-146.
[22]Cao Licheng.Provenance evolution since Neogene in the Yinggehai and Qiongdongnan Basins:Evidence from REE,heavy minerals and zircon U-Pb ages[D].Beijing:China University of Geosciences,2014.[曹立成.莺歌海—琼东南盆地区新近纪物源演化研究[D].北京:中国地质大学,2014.]
[23]Shao L,Cao L C,Pang X,et al.Detrital zircon provenance of the Paleogene syn-rift sediments in the northern South China Sea[J].Geochemistry Geophysics Geosystems,2016,17(2) :255-269.
[24]Hoang L V,Wu F Y,Clift P D,et al.Evaluating the evolution of the Red River System based on in situ U-Pb dating and Hf isotope analysis of zircons[J].Geochemistry Geophysics Geosystems,2009,10(11):292-310.
[25]Burrett C,Zaw K,Meffre S,et al.The configuration of Greater Gondwana-Evidence from LA ICPMS,U-Pb geochronology of detrital zircons from the Palaeozoic and Mesozoic of Southeast Asia and China[J].Gondwana Research,2013,26(1):1-51.