[1] Chen Changmin, Pang Xiong. The deep-water lowstand fan and its exploration potential of the Pearl River Mouth Basin (PRMB)[C]. Paper to the World Petroleum Congresses Asia Regional Meeting.Shanghai, 2001,(CD version).

[2] Pang Xiong, Yang Shaokun, Zhu Ming, et al. The deep-water fan systems and petroleum resource in northern slope of South China Sea[J]. Acta Geologica Sinica (English edition), 2004, 78(3):626-631.

[3] Pang Xiong,Chen Changmin,Shi Hesheng, et al. Response between relative sea-level change and the Pearl River deepwater fan system in the South China Sea[J]. Earth Science Frontiers,2005,12(3):167-177.[庞雄,陈长民,施和生,等.相对海平面变化与南海珠江深水扇系统的响应[J].地学前缘,2005,12(3):167-177.]

[4] Peng Dajun, Chen Changmin, Pang Xiong, et al. Discovery of deep-water fan system in South China Sea[J]. Acta Petrolei Sinica, 2004, 25(1):17-23.[彭大钧,陈长民,庞雄,等.南海珠江口盆地深水扇系统的发现[J].石油学报,2004,25(1):17-23.]

[5] Peng Dajun, Pang Xiong, Chen Changmin, et al. From shallow-water shelf to deep-water slope—The research of deepwater fan systems in south China sea[J]. Acta Sedimentologica Sinica, 2005, 23(1):1-11.[彭大钧,庞雄,陈长民,等.从浅水陆架走向深水陆坡—南海深水扇系统的研究[J].沉积学报,2005,23(1):1-11.]

[6] Pang Xiong, Chen Changmin, Peng Dajun, et al. Sequence stratigraphy of Pearl river deep-water fan systems of the south China sea[J]. Earth Science Frontiers, 2006, 13:in press.[庞雄,陈长民,彭大钧,等.南海珠江深水扇系统的层序地层学研究[J].地学前缘,2006,13(待刊).]

[7] Liu Guangding. Map Series of Geology and Geophysics of China Seas and Adjacent Regions[M]. Beijing: Geological Publishing House,1992.[刘光鼎主编.中国海区及邻域地质—地球物理系列图[M].北京:地质出版社,1992.]

[8] Shao Lei, Li Xianhua, Wang Pinxian, et al. Sedimentary record of the tectonic evolution of the south China sea since the Oligocene—Evidence from deep sea sediments of ODP site 1148[J]. Advances in Earth Science, 2004,19(4):539-544.[邵磊,李献华,汪品先,等.南海渐新世以来构造演化的沉积记录——ODP1148站深海沉积物中的证据[J].地球科学进展,2004,19(4): 539-544.]

[9] Li Qianyu, Zheng Hongbo, Zhong Guangfa, et al. Tectonic events indicated by Late Oligocene slumped deposits from the south China sea[J]. Earth Science—Journal of China University of Geosciences,2005,30(1):19-24.[李前裕,郑洪波,钟广法,等. 南海晚渐新世滑塌沉积指示的地质构造事件[J]. 地球科学——中国地质大学学报,2005, 30(1):19-24.]

[10] Shao Lei,Lei Yongchang,Pang Xiong,et al. Tectonic evolution and its controlling for sedimentary environment in Pearl river mouth basin[J]. Journal of Tongji University (Natural Science),2005, 33(9):1 177-1 181.[邵磊,雷永昌,庞雄,等.珠江口盆地构造演化及对沉积环境的控制作用[J].同济大学学报:自然科学版, 2005, 33(9):1 177-1 181.]

[11] Wang Pinxian, Zhao Quanhong, Jian Zhimin, et al. Thirty million year deep-sea records in the south China sea[J]. Chinese Science Bulletin, 2003, 48(21):2 206-2 215.[汪品先,赵泉鸿,翦知湣,等.南海三千万年的深海记录[J].科学通报,2003,48(21): 2 206-2 215.]

[12] Pang Xiong, Chen Changmin, Shao Lei, et al. Great tectonic event on the Oligocence/Miocene boundary in the northern South China sea and its implications[J]. Acta Geologica Sinica, 2006, in press.[庞雄,陈长明,邵磊,等.南海北部渐新统/中新统重大地质事件及意义[J].地质学报,2006(待刊).]

[13] Clift P, Lee J I, Clark M K, et al. Erosional response of South China to arc rifting and monsoonal strengthening: A record from the south China sea[J]. Marine Geology,2002, 184:207-226.

[14] Wang Chengshan, Ding Xuelin. The new researching progress of Tibet plateau Up lift[J]. Advances in Earth Science,1998,13(6):526-532.[王成善,丁学林. 青藏高原隆升研究新进展综述[J]. 地球科学进展,1998,13(6):526-532.]

[15] Dewey J F, Shackleton R M, Cheng Chengfa, et al. Tectonic evolution of Qinghai-Xizang Plateau,Geology Evolution of Qinghai-Xizang Plateau[M]. Beijing: Science Press, 1990:384-415.[Dewey J F, Shackleton R M,常承法,等. 青藏高原的构造演化.青藏高原地质演化[M]. 北京:科学出版社, 1990:384-415.]

[16] Li Tingdong. The uplifting process and mechanism of the Qinghai-Tibet plateau[J]. Acta Geoscientia Sinic,1995, (1):1-9.[李廷栋. 青藏高原隆升的过程和机制[J]. 地球学报, 1995, (1):1-9.]

[17] Shi Yafeng, Li Jijun, Li Bingyuan. Up lift and Environmental Change of Tibet Plateau in Late Cenozoic Era[M]. Guangzhou: Guangdong Science & Technology Press, 1998. [施雅风,李吉均,李炳元. 青藏高原晚新生代隆起与环境变化[M]. 广州:广东科技出版社, 1998.]

[18] Zhong Dalai, Ding Lin. Up lifted process and its mechanism of the Tibet plateau[J]. China Science (D), 1996, 26 (4):289-295[钟大赉,丁林. 青藏高原的隆起过程及其机制探讨[J]. 中国科学:D辑, 1996, 26(4):289-295.]

[19] Fan Daidu, Li Congxian, K.Yokoyama, et al. The Research of age spectrum of monazite in the Neogene Yangtse river delta and Yangtse river through time[J]. Science in China (Series D),2004,34(11):1 015-1 022. [范代读,李从先,K.Yokoyama,等.长江三角洲晚新生代地层独居石年龄谱与长江贯通时间研究[J].中国科学:D辑,2004,34(11):1 015-1 022.]

[20] Li J J, Xie S Y, Kuang M S. Geomorphic evolution of the Yangtze Gorges and the time of their formation[J]. Geomorphology, 2001, 41:125-135.

[21] Clark M K, Schoenbohm L M, Royden L H, et al. Surface uplift, tectonics, and erosion of eastern Tibet from large-scale drainage patterns[J]. Tectonics,2004,23:TC1006, 1-20.

[22] Zhu Jieshou,Cao Jiamin,Cai Xuelin,et al. High resolution surface wave tomography in east Asia and west Pacific marginal seas [J]. Chinese Journal of Geophysics,2002,45(5):646-664.[朱介寿,曹家敏,蔡学林,等. 东亚及西太平洋边缘海高分辨率面波层析成像[J].地球物理学报,2002,45(5):646-664.]

[23] Gong Zaisheng, Li Sitian, et al. Continental Margin Basin Analysis and Hydrocarbon Accumulation of the Northern South China Sea[M] Beijing: Science Press, 1997:1-510.[龚再升,李思田,等.南海北部大陆边缘盆地分析与油气聚集[M].北京:科学出版社,1997.]

[24] Briais A, Patriat P, Tapponnier P. Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea, implications for the Tertiary tectonics of Southeast Asia[J]. Journal of Geophysical Research, 1993, 98:6 299-6 328.

[25] Huang Chunju, Zhou Di, Chen Changmin, et al. Deep crust architecture exposed by deep reflecting seismic profile in Baiyun sag[J]. Chinese Science Bulletin,2005, 50(10):1 024-1 031.[黄春菊,周蒂,陈长民,等.深反射地震剖面所揭示的白云凹陷的深部地壳结构[J].科学通报,2005, 50(10):1 024-1 031.]

[26] Wu Xiangjie,Zhou Di,Pang Xiong,et al. Geophysical field and deep structures of Baiyun sag, Pearl river mouth basin[J]. Journal of Tropical Oceanography,2005, 24(2):62-69. [吴湘杰,周蒂,庞雄,等.白云凹陷地球物理场及深部结构特征[J]. 热带海洋学报,2005, 24(2):62-69.]

[27] Sun Zhen, Pang Xiong, Zhong Zhihong, et al. Dynamics of Tertiary tectonic evolution of the Baiyun sag in the Pearl river mouth basin[J]. Earth Science Frontiers,2005,12(4):489-498.[孙珍,庞雄,钟志洪,等.珠江口盆地白云凹陷新生代构造演化动力学[J].地学前缘,2005,12(4):489-498.]

[28] Peng Dajun, Pang Xiong, Chen Changmin, et al. The characteristics and controlling factors for the formation of deep-water fan system in south China sea[J]. Acta Sedimentologica Sinica,2006,24(1):10-18.[彭大钧,庞雄,陈长民,等. 南海珠江深水扇系统的形成特征与控制因素[J]. 沉积学报,2006,24(1):10-18.]

[29] Qin Guoquan. Late Cenozoic sequence stratigraphy and sea-level changes in Pearl river mouth basin, south China sea[J]. China Offshore Oil and Gas(Geology), 2002, 16(1):1-10.[秦国权. 珠江口盆地新生代晚期层序地层划分和海平面变化[J].中国海上油气(地质), 2002,16(1):1-10.]

[30] Chen Zhongqiang, Zhong Shilan, Yang Shaokun, et al. The application of micropalaeontology in sequence stratigraphy: An example from the Huizhou depression in south China sea[J]. Acta Micropalaeontologica Sinica,1998,15(2):134-143.[陈中强,钟石兰,杨少坤,等. 微古生物在高分辨层序地层学中的应用——以珠江口盆地惠州凹陷层序地层分析为例[J]. 微体古生物学报,1998,15 (2):134-143.]

[31] Qin Guoquan. Application of micropaleontology in the Late Cenozoic sequence stratigraphy study of the Pearl river mouth basin[J]. Ocean Geology and Quarternary Geology, 1996, 16(4):1-18. [秦国权.微体古生物在珠江口盆地新生代晚期层序地层学研究中的运用[J].海洋地质与第四纪地质,1996, 16(4):1-18.]

[32] Haq B U, Hardenbo L J, Vail P R. Mesozoic and Cenozoic chronostratigraphy and cycles of sea level change[C]∥Wilgus C K, et al. Sea Level Change: An Integrated Approach. Society of Econonic Paleontologists and Mineralogists Special Publication, 1988, 42:71-108.

[33] Cochran J R. Himalayan uplift, sea level. and the record of Bengal fan sedimentation at the ODP Leg116 sites[C]∥Cochran J R, Stow D A V, et al, eds. Scientific Results Ocean Drilling Program. 1990, 116: 397-414.

[34] Wang Pinxian. ODP and Qinghai/Xizang(Tibetan) plateau[J]. Advances in Earth Science,1995,10(3):254-257.[汪品先.大洋钻探与青藏高原[J]. 地球科学进展,1995,10(3):254-257.]