Sedimentary Facies and Evolution of Tectonic Environments in the Jinhua-Quzhou Basin,Zhejiang Province

ZU Fu-ping; LI Cheng; WANG Bin

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(3): 417-424

ZU Fu-ping, LI Cheng, WANG Bin. Sedimentary Facies and Evolution of Tectonic Environments in the Jinhua-Quzhou Basin,Zhejiang Province[J]. Acta Sedimentologica Sinica, 2004, 22(3): 417-424.

Citation:

ZU Fu-ping, LI Cheng, WANG Bin. Sedimentary Facies and Evolution of Tectonic Environments in the Jinhua-Quzhou Basin,Zhejiang Province[J]. Acta Sedimentologica Sinica, 2004, 22(3): 417-424.

Sedimentary Facies and Evolution of Tectonic Environments in the Jinhua-Quzhou Basin,Zhejiang Province

Department of Earth Science, Nanjing University, Nanjing 210093

Received Date: 2003-06-10
Rev Recd Date: 2003-10-09
Publish Date: 2004-09-10

Abstract

Jinhua-QuzhouBasin developed on the metamorphosed basement of Palaeozoic fold, and its formation and development was greatly influenced by pre-mesozoic tectonic framework and geological characteristics. In this paper, the author studied paleogeographic environment, sedimentary structure, depocenter and paleolithological changes etc., analyzed Jinhua-Quzhou Basin's history of formation and evolution and discussed its evolution of tectonic setting from Late-Mesozoic to Cenozoic. From what was studied, four conclusions have been reached: ①Jinhua-Quzhou basin was a fault basin because of compression and then extention; and its boundaries were mostly normal faults. ②In different areas of the basin, there were different stratigraphic sequences. ③Sedimentary facies: the distribution of Jinhua-Quzhou Basin's sedimentary facies varied in different stages, and to some extent, the evolution sequences were clear. Alluvial fan facies spread in northern and southern borders of Jinhua-Quzhou basin as alluvial fan apron with some differences. River facies and sand bank facies distributed in the middle of Jinhua-Quzhou Basin, locating in sectors between Quxian and Longyou. Delta facies included fan delta, braided delta and normal delta. Also, in areas we studied, there were lake facies, but shore shallow lake subfacies and semi-deep lake subfacies were the most important ones.
- sedimentary facies,
- depocenter,
- tectonic environment,
- Jinhua-Quzhou Basin

References

[1]	刘和甫.盆地演化与地球动力学旋回.地学前缘,1997,4(3-4):233～240[Liu Hefu.Evolution of basins related to geodynamic cycles. Earth Science Frontiers, 1997, 4(3-4):233～240]
[2]	舒良树,周新民.中国东南部晚中生代构造作用.地质论评,2002,48(3):249～260[Shu Liangshu, Zhou Xinmin.Late Mesozoic Tectonism of Southeast China. Geological Review, 2002, 48(3):249～260]
[3]	刘和甫.沉积盆地地球动力学分类及构造样式分析.地球科学,1993,18(6):699～724[Liu Hefu. Dynamic classification of sedimentary basins and their structural styles. Earth Science, 1993, 18(6):699～724]
[4]	熊绍柏,赖明惠,刘宏宾,等.屯溪-温州地带岩石圈结构与速度分布.见:李继亮主编,东南大陆岩石圈结构与地质演化.北京:冶金工业出版社,1993.250～256[Xiong Shaobo, Lai Minghui, Liu Hongbin, et al. Lithosphere Framework and Velocity Distribution of Tunxi-Wenzhou Belt. In: Li Jiliang ed. Lithosphere Framework and Geological Evolution of Southeastern Mainland of China. Beijing: Publishing House of Metallurgy Industry, 1993.250～256]
[5]	田在艺,张庆春.沉积盆地控制油气赋存的因素.石油学报,1993,14 (4):1～19[Tian Zaiyi, Zhang Qingchun. Factors controlling oil and gas occurrence in a sedimentary basin. Acta Petrolei Sinica, 1993, 14(4):1～19]
[6]	陈溥鹤.断裂系统在油气成藏中的应用.海相油气地质,1998,3(4):1～2[Chen Fuhe.The application of fracture system in petroleum accumulation. Petroleum Geology of Marine Facies, 1998, 3(4):1～2]
[7]	Gilder S A, Keller G R, Luo Ming, et al. Eastern Asia and the western Pacific timing and spatial distribution of rifting in China. Tectonophysics, 1991, 197: 225～243
[8]	浙江省地质矿产局.浙江省区域地质志.北京:地质出版社,1989.1～921[Geological Bureau of Zhejiang Province. Regional Geology Records of Zhejiang Province. Beijing: Geological Publishing House, 1989.1～921]
[9]	浙江省地质矿产局.浙江省岩石地层.武汉:中国地质大学出版社,1996. 1～236[Geological and Ore Bureau of Zhejiang Province. Rock Stratum of Zhejiang Province. Wuhan:The Press of Geology University of China, 1996. 1～236]
[10]	张星蒲.赣杭构造带中生代火山盆地的形成和演化.铀矿地质,1999,15(1):18～23[Zhang Xingpu. Formation and evolution of Mesozoic volcanic basins in Gan-Hang tectonic belt. Uranium Geology, 1999, 15(1):18～23]
[11]	刘和甫.中国沉积盆地演化与旋回动力学环境.地球科学,1996,21(4):345～356[Liu Hefu. Cycle-Geodynamic scenario and evolution of sedimentary basins in China. Earth Science, 1996, 21(4):345～356]
[12]	张星蒲.赣杭构造带中生代红色碎屑沉积盆地的形成和演化.铀矿地质,1999,15(2):77～85[Zhang Xingpu. Formation and evolution of Mesozoic red basins in Gan-Hang tectonic belt. Uranium Geology, 1999, 15(2):77～85]
[13]	吕学斌.金衢盆地沉积环境演变.山地研究,1993,11(1):15～22[Lü Xuebin. Evolution of sedimentary environment of Jinhua-Quzhou Basin, Zhejiang Province. Mountain Research, 1993, 11(1):15～22]
[14]	Okada H. Plume-related sedimentary basins in East Asia during the Cretaceous. Palaeogeography, Palaeoclimatology, Palaeoecology,1999,150:1～11.
[15]	张春生,刘忠保,施冬,等.扇三角洲形成过程及演变规律.沉积学报, 2000, 18(4):521～526[Zhang Chunsheng, Liu Zhongbao, Shi Dong, et al. Formed proceeding and evolution disciplinarian of fan delta. Acta Sedimentologica Sinica, 2000, 18(4):521～526]
[16]	Pirajno F, Bagas L, Hickman A H. Gold Research Team. Gold mineralization of the Chencai-Suichang Uplift and tectonic evolution of Zhejiang Province, southeast China. Ore Geol. Rev.,1997,12:35～55.
[17]	刘文庆,胡忠行.金衢盆地自然环境演化基本特点与趋势.浙江师大学报(自然科学版),1994,17(3):23～29[Liu Wenqing, Hu Zhongxing. The basic evolution features and development trend of natural environment in Tin-Qu Basin. Journal of Zhejiang Normal University (Nature Science), 1994, 17(3): 23～29]
[18]	Shu L.-S, and Jacques C. Kinematic and geochronology of the Proterozoic Dongxiang-Shexian ductile shear zone (Jiangnan region, South China). Tectonophysics, 1996, 267(1-4): 291～302.
[19]	舒良树,卢华复,Charvet J, Faure M. 武夷山北缘断裂带运动学研究.高校地质学报, 1997,3(3):282～292[Shu Liangshu, Lu Huafu,Charvet J, Faure M. Kinematic study of the northern marginal fault zone of Wuyishan, south China. Geological Journal of China Universities, 1997, 3(3): 282～292]
[20]	Engebretson D C, Cox A and Gordon R G. Relative motions between oceanic and continental plates in the Pacific basin. Geol Soc Am Spec Paper,1985, 1～59.
[21]	Maruyama S, Isozaki Y, Kimura G and Terabayashi M. Paleogeographic maps of the Japanese islands: plate tectonic synthesis from 750 Ma to the present. The Island Arc, 1997, 6(1): 121～142
[22]	舒良树,于津海,王德滋.长乐-南澳断裂带晚中生代岩浆活动与变质-变形特征.高校地质学报,2000,6(3):368～378.[Shu Liangshu, Yu Jinhai, Wang Dezi. Late Mesozic grantic magmatism and metamorphism-ductile deformation in the Changle-Nanao fault zone, Fujian Province. Geological Journal of China Universities,2000,6(3): 368～378]

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通讯作者: 陈斌, bchen63@163.com

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Sedimentary Facies and Evolution of Tectonic Environments in the Jinhua-Quzhou Basin,Zhejiang Province

Department of Earth Science, Nanjing University, Nanjing 210093

Received Date: 2003-06-10

Rev Recd Date: 2003-10-09

Publish Date: 2004-09-10

Key words:

Abstract: Jinhua-QuzhouBasin developed on the metamorphosed basement of Palaeozoic fold, and its formation and development was greatly influenced by pre-mesozoic tectonic framework and geological characteristics. In this paper, the author studied paleogeographic environment, sedimentary structure, depocenter and paleolithological changes etc., analyzed Jinhua-Quzhou Basin's history of formation and evolution and discussed its evolution of tectonic setting from Late-Mesozoic to Cenozoic. From what was studied, four conclusions have been reached: ①Jinhua-Quzhou basin was a fault basin because of compression and then extention; and its boundaries were mostly normal faults. ②In different areas of the basin, there were different stratigraphic sequences. ③Sedimentary facies: the distribution of Jinhua-Quzhou Basin's sedimentary facies varied in different stages, and to some extent, the evolution sequences were clear. Alluvial fan facies spread in northern and southern borders of Jinhua-Quzhou basin as alluvial fan apron with some differences. River facies and sand bank facies distributed in the middle of Jinhua-Quzhou Basin, locating in sectors between Quxian and Longyou. Delta facies included fan delta, braided delta and normal delta. Also, in areas we studied, there were lake facies, but shore shallow lake subfacies and semi-deep lake subfacies were the most important ones.

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Reference (22)

[1]	刘和甫.盆地演化与地球动力学旋回.地学前缘,1997,4(3-4):233～240[Liu Hefu.Evolution of basins related to geodynamic cycles. Earth Science Frontiers, 1997, 4(3-4):233～240]
[2]	舒良树,周新民.中国东南部晚中生代构造作用.地质论评,2002,48(3):249～260[Shu Liangshu, Zhou Xinmin.Late Mesozoic Tectonism of Southeast China. Geological Review, 2002, 48(3):249～260]
[3]	刘和甫.沉积盆地地球动力学分类及构造样式分析.地球科学,1993,18(6):699～724[Liu Hefu. Dynamic classification of sedimentary basins and their structural styles. Earth Science, 1993, 18(6):699～724]
[4]	熊绍柏,赖明惠,刘宏宾,等.屯溪-温州地带岩石圈结构与速度分布.见:李继亮主编,东南大陆岩石圈结构与地质演化.北京:冶金工业出版社,1993.250～256[Xiong Shaobo, Lai Minghui, Liu Hongbin, et al. Lithosphere Framework and Velocity Distribution of Tunxi-Wenzhou Belt. In: Li Jiliang ed. Lithosphere Framework and Geological Evolution of Southeastern Mainland of China. Beijing: Publishing House of Metallurgy Industry, 1993.250～256]
[5]	田在艺,张庆春.沉积盆地控制油气赋存的因素.石油学报,1993,14 (4):1～19[Tian Zaiyi, Zhang Qingchun. Factors controlling oil and gas occurrence in a sedimentary basin. Acta Petrolei Sinica, 1993, 14(4):1～19]
[6]	陈溥鹤.断裂系统在油气成藏中的应用.海相油气地质,1998,3(4):1～2[Chen Fuhe.The application of fracture system in petroleum accumulation. Petroleum Geology of Marine Facies, 1998, 3(4):1～2]
[7]	Gilder S A, Keller G R, Luo Ming, et al. Eastern Asia and the western Pacific timing and spatial distribution of rifting in China. Tectonophysics, 1991, 197: 225～243
[8]	浙江省地质矿产局.浙江省区域地质志.北京:地质出版社,1989.1～921[Geological Bureau of Zhejiang Province. Regional Geology Records of Zhejiang Province. Beijing: Geological Publishing House, 1989.1～921]
[9]	浙江省地质矿产局.浙江省岩石地层.武汉:中国地质大学出版社,1996. 1～236[Geological and Ore Bureau of Zhejiang Province. Rock Stratum of Zhejiang Province. Wuhan:The Press of Geology University of China, 1996. 1～236]
[10]	张星蒲.赣杭构造带中生代火山盆地的形成和演化.铀矿地质,1999,15(1):18～23[Zhang Xingpu. Formation and evolution of Mesozoic volcanic basins in Gan-Hang tectonic belt. Uranium Geology, 1999, 15(1):18～23]
[11]	刘和甫.中国沉积盆地演化与旋回动力学环境.地球科学,1996,21(4):345～356[Liu Hefu. Cycle-Geodynamic scenario and evolution of sedimentary basins in China. Earth Science, 1996, 21(4):345～356]
[12]	张星蒲.赣杭构造带中生代红色碎屑沉积盆地的形成和演化.铀矿地质,1999,15(2):77～85[Zhang Xingpu. Formation and evolution of Mesozoic red basins in Gan-Hang tectonic belt. Uranium Geology, 1999, 15(2):77～85]
[13]	吕学斌.金衢盆地沉积环境演变.山地研究,1993,11(1):15～22[Lü Xuebin. Evolution of sedimentary environment of Jinhua-Quzhou Basin, Zhejiang Province. Mountain Research, 1993, 11(1):15～22]
[14]	Okada H. Plume-related sedimentary basins in East Asia during the Cretaceous. Palaeogeography, Palaeoclimatology, Palaeoecology,1999,150:1～11.
[15]	张春生,刘忠保,施冬,等.扇三角洲形成过程及演变规律.沉积学报, 2000, 18(4):521～526[Zhang Chunsheng, Liu Zhongbao, Shi Dong, et al. Formed proceeding and evolution disciplinarian of fan delta. Acta Sedimentologica Sinica, 2000, 18(4):521～526]
[16]	Pirajno F, Bagas L, Hickman A H. Gold Research Team. Gold mineralization of the Chencai-Suichang Uplift and tectonic evolution of Zhejiang Province, southeast China. Ore Geol. Rev.,1997,12:35～55.
[17]	刘文庆,胡忠行.金衢盆地自然环境演化基本特点与趋势.浙江师大学报(自然科学版),1994,17(3):23～29[Liu Wenqing, Hu Zhongxing. The basic evolution features and development trend of natural environment in Tin-Qu Basin. Journal of Zhejiang Normal University (Nature Science), 1994, 17(3): 23～29]
[18]	Shu L.-S, and Jacques C. Kinematic and geochronology of the Proterozoic Dongxiang-Shexian ductile shear zone (Jiangnan region, South China). Tectonophysics, 1996, 267(1-4): 291～302.
[19]	舒良树,卢华复,Charvet J, Faure M. 武夷山北缘断裂带运动学研究.高校地质学报, 1997,3(3):282～292[Shu Liangshu, Lu Huafu,Charvet J, Faure M. Kinematic study of the northern marginal fault zone of Wuyishan, south China. Geological Journal of China Universities, 1997, 3(3): 282～292]
[20]	Engebretson D C, Cox A and Gordon R G. Relative motions between oceanic and continental plates in the Pacific basin. Geol Soc Am Spec Paper,1985, 1～59.
[21]	Maruyama S, Isozaki Y, Kimura G and Terabayashi M. Paleogeographic maps of the Japanese islands: plate tectonic synthesis from 750 Ma to the present. The Island Arc, 1997, 6(1): 121～142
[22]	舒良树,于津海,王德滋.长乐-南澳断裂带晚中生代岩浆活动与变质-变形特征.高校地质学报,2000,6(3):368～378.[Shu Liangshu, Yu Jinhai, Wang Dezi. Late Mesozic grantic magmatism and metamorphism-ductile deformation in the Changle-Nanao fault zone, Fujian Province. Geological Journal of China Universities,2000,6(3): 368～378]

Sedimentary Facies and Evolution of Tectonic Environments in the Jinhua-Quzhou Basin,Zhejiang Province

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