Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

MEI Ming-xiang; GAO Jin-han; LI Dong-hai; MENG Qing-fen; YI Ding-hong

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2003 > 21(2): 297-306

MEI Ming-xiang, GAO Jin-han, LI Dong-hai, MENG Qing-fen, YI Ding-hong. Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China[J]. Acta Sedimentologica Sinica, 2003, 21(2): 297-306.

Citation:

Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

Faculty of Earth Sciences and Resources, China University of Geosciences, Beijing 100083

Received Date: 2002-02-05
Rev Recd Date: 2002-05-08
Publish Date: 2003-06-10

Abstract

There is a great change of paleogeography setting resulted from the Caledonian orogeny at the end of Silurian in Guizhou and Guangxi area in south China, the Dianqiangui oldland in early Paleozoic evolved as the Dianqiangui sea in late Plaeozoic. In the initial stage of Devonian Period, seawater is onlaped gradually from the south to the north caused by transgression, so the bottom part of Devonian system is constituted by a set of transgressive clastic sedimentary rock. The great scale transgressive event at the end of the early Epoch of Devonian forms evident differentiation of depositional facies in Guizhou and Guangxi province, a lot of isolated carbonate platforms are developed in Dianqiangui Basin, the special paleogeographic setting marked by "platforms-basins-hills-trough" is formed and lasted to the early stage of the late Epoch of Devonian. The strata of the upper Epoch of Devonian become regressive thin out from paleosea to oldland resulted from the Ziyun epeirogeny that took place in the transitional period from Devonian Period to Carboniferous Period. On the basis of the study on the evolutional natures of sediments in time and the distribution characters of sedimentary facies in space, 13 third-order sedimentary sequences are discerned in Devonian strata in Guizhou and Guangxi province, which could be grouped into one second-order tectonic sequence. In terms of the correlation on biostratigraphy, the sea-level changes delegated by third-order sequences with different architecture natures of facies-succession also could be correlative in research region, in the end, the framework of sequence stratigraphy could be constructed. Many characters such as two elementary natures of third-order sequences——“the regularity of facies-succession in space and the synchronism of the changes of sedimentary environment in time”, two kinds of diachronism that are relative to two types of facies-changing surfaces——“the diachronism of facies-changing surfaces caused by static facies-changing surface and the diachronism of punctuated surfaces formed by dynamic facies-changing surfaces" in strtigraphic records, are clearly demonstrated in the framework of sequence stratigraphy.
- the framework of sequence stratigraphy,
- Devonian system,
- Guizhou and Guangxi area in south China

References

[1]	侯鸿飞,曹宣铎,王士涛,鲜思远,王金星.中国地层典(泥盆系)[M].北京:地质出版社,2000.1～118[Hou Hongfei,Cao Xuanduo, Wang Shitao, Xian Siyuan, Wang Jinxing. Chinese stratigraphic lexicon ( Devonian system)[M]. Beijing: Geological Publishing House,2000.1 ～ 118
[2]	赵自强,丁启秀主编.中南区区域地层[M].武汉:中国地质大学出版社,1996.71～123[Zhao Ziqiang,Ding Qixiu.The regional stratigraphy in central and south part of China[M]. Wuhan: China U-niversity of Geosienes Press,1996 71～123]
[3]	董卫平主编.贵州省岩石地层[M].武汉:中国地质大学出版社,1997. 143 ～ 220 [Dong Weiping. Lithostratigraphy in Guizhou [M].Wuhan: China University of Geosciences Press, 1997. 143～220]
[4]	殷保安主编.广西状族自治区岩石地层[M].武汉:中国地质大学出版社,1997 52～191[Yin Baoan.Lithostratigraphy in Guangxi[M].Wuhan:China University of Geosciences Press,1997.52～191]
[5]	曾允乎,张锦泉,刘文均等.中国南方泥盆纪岩相古地理与成矿作用[M].北京:地质出版社,1994.1～120[Zen Yunfu,Zhang Jinquan, Liu Wenjun, Zhou Huailin, Chen Hongde. Devonian lithofacies paleogeography and mineralization in south China[M]. Beijing: Geological Publishing House, 1994. 1～120]
[6]	吴诒,周怀玲,蒋廷操等.广西泥盆纪沉积相古地理及矿产[M].南宁:广西人民出版社,1987.1～256[Wu Yi,Zhou Huailing,Jiang Tingchao Fang Daonian, Huang Wusheng. The sedimentary facies paleogeography and relatively mineral deposits of Devonian in Guangxi[M].Nanning: Guangxi Peoples Publishing Hoase, 1987.1 ～256]
[7]	钟铿,吴诒,殷保安等.广西的泥盆系[M].武汉:中国地质大学出版社,1992.1～370[Zhong Keng,Wu Yi,YinBaoan,et al.Devonian systen of Guangxi[M]. Wuhan: China University of Geosciences Press, 1992. 1～370]
[8]	邝网敦,赵明特,陶业斌编著广西六景泥盆系剖面[M].武汉:中国地质大学出版社,1989.1～155[Kuang Guodun,Zhao Mingte,Tao Yebin. The standard Devonian section of China: Liujing section of Guangxi[M]. Wuhan: China University of Geosciences Press, 1989.1～154]
[9]	许效松,牟传龙,林明著.露头层序地层与华南泥盆纪古地理[M].成都:成都科技大学出版社,1993.1～288[Xu Xiaosong,Mou Chuanlong, Lin Ming. The outcrop sequence stratigraphy of Devonian and palcogeography in south-China[M]. Chengdu: Chengdu University of Sciencs and Technology Press, 1993. 1 ～288]
[10]	吴诒,龚一鸣,杜远生.华南泥盆纪层序地层及海平面变化[M].武汉:中国地质大学出版社,1997.1～98[Wu Yi,Du Yuansheng,Gong Yiming. Devonian sequenoe stratigraphy and the relative sea-lev-el changes in South-China [M]. Wuban: China University of Geosciences Press, 1997. 1～98]
[11]	杨惠民,刘炳温,邓宗怀等.滇黔桂海相碳酸盐岩地区最佳油气保存单元的评价与选择[M].贵阳:贵州科技出版社,1999.4～63[Yang Huiming, Liu Binwen, Deng Zonghuai, et al. Value and Selection to the Best Gas-Oil Keeping Unite of Marine Carbonate Area in Yunnan, Guizhou and Guangxi[M]. Guiyang: Guizhou Science and Technology Press, 1999. 4 ～63]
[12]	梅冥相,马永生,戴少武等.南盘江盆地晚古生代盆地充填序列特征及生储盖组合划分[J].现代地质,2001,15(1):74～82[Mei Mingxiang, Ma Yongsheng, Dai Shaowu, et al. Late Paleozoic filling succession of the Dianqiangui Basin and the division of association of oilgenerating strata, reservoir, and capping bed[J]. Geosciences,2001,15(1), 74～82]
[13]	吴浩若.广西加里东运动构造古地理问题[J].古地理学报,2000,2(1): 70 ～ 76 [Wu Haoruo. A discussion on the tectonic paleogeography related to the Caledonian movement in Guangxi[J]. Journal of Paleogeography, 2000,2(1): 70～76]
[14]	陈旭,阮亦萍,AJ布科主编,中国古生代气候演变[M].北京:科学出版社,2001 40～53[Chen Xu,Ruan Yiping,A J Boucot.The climate evolution of Plaeozoic in China [M]. Beijing: Sciences Press, 2001, 40～53]
[15]	梅冥相,马永生.从旋回层序的特征论地层记录的两种相变面及两种穿时性[J].地层学杂志,2001,25(2):150～153[Mei Mingxiang, Ma Yongsheng. On two kinds of Facies-change surface and two kinds of diachronisa in stratigraphical records according to the natures of cyclic-sequences[J]. Journal of Stratigraphy, 2001,25(2): 150-153]
[16]	梅冥相.从地层记录的特征论岩石地层学的困惑[J].地层学杂志,1996,20(3):207～212[Mei Mingxiang.On the perplexity of lithostratigraphy according to the natures of stratigraphic records[J].Journal of Stratigraphy, 1996, 20(3): 207～212]
[17]	周希云.贵州泥盆纪几个地层问题的讨论[J].贵州地质,1992,9(4): 331～339[Zhou Xiyun. On discussion of the several problens on Devonian stratigraphy[J]. Guizhou Geology, 1992, 9 (4): 331 ～339]
[18]	Enos P , Wei Jiayong, Lehrmann D J. Death in Guizhou-Late Triassic dromning of the Yangtze carbonate platform[J]. Sedimentary Geology, 1998, 118:55～76
[19]	Johson J G, Klapper G. North American Midcontinent Devonian T-R cycles[J]. Oklahoma Geological Survey Bulletin, 1992,145: 127～135
[20]	Ross C A, Ross J R P. Late Paleozoic transgressive-regressive deposition[A]. In: Wilgus C K, ed. Sea-level Changes: an Integrated Aptoroach[C]. SEPM Spec Pub, 1988, 42:227～247

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通讯作者: 陈斌, bchen63@163.com

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Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

Faculty of Earth Sciences and Resources, China University of Geosciences, Beijing 100083

Received Date: 2002-02-05

Rev Recd Date: 2002-05-08

Publish Date: 2003-06-10

Key words:

the framework of sequence stratigraphy /
Devonian system /
Guizhou and Guangxi area in south China

Abstract: There is a great change of paleogeography setting resulted from the Caledonian orogeny at the end of Silurian in Guizhou and Guangxi area in south China, the Dianqiangui oldland in early Paleozoic evolved as the Dianqiangui sea in late Plaeozoic. In the initial stage of Devonian Period, seawater is onlaped gradually from the south to the north caused by transgression, so the bottom part of Devonian system is constituted by a set of transgressive clastic sedimentary rock. The great scale transgressive event at the end of the early Epoch of Devonian forms evident differentiation of depositional facies in Guizhou and Guangxi province, a lot of isolated carbonate platforms are developed in Dianqiangui Basin, the special paleogeographic setting marked by "platforms-basins-hills-trough" is formed and lasted to the early stage of the late Epoch of Devonian. The strata of the upper Epoch of Devonian become regressive thin out from paleosea to oldland resulted from the Ziyun epeirogeny that took place in the transitional period from Devonian Period to Carboniferous Period. On the basis of the study on the evolutional natures of sediments in time and the distribution characters of sedimentary facies in space, 13 third-order sedimentary sequences are discerned in Devonian strata in Guizhou and Guangxi province, which could be grouped into one second-order tectonic sequence. In terms of the correlation on biostratigraphy, the sea-level changes delegated by third-order sequences with different architecture natures of facies-succession also could be correlative in research region, in the end, the framework of sequence stratigraphy could be constructed. Many characters such as two elementary natures of third-order sequences——“the regularity of facies-succession in space and the synchronism of the changes of sedimentary environment in time”, two kinds of diachronism that are relative to two types of facies-changing surfaces——“the diachronism of facies-changing surfaces caused by static facies-changing surface and the diachronism of punctuated surfaces formed by dynamic facies-changing surfaces" in strtigraphic records, are clearly demonstrated in the framework of sequence stratigraphy.

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Reference (20)

[1]	侯鸿飞,曹宣铎,王士涛,鲜思远,王金星.中国地层典(泥盆系)[M].北京:地质出版社,2000.1～118[Hou Hongfei,Cao Xuanduo, Wang Shitao, Xian Siyuan, Wang Jinxing. Chinese stratigraphic lexicon ( Devonian system)[M]. Beijing: Geological Publishing House,2000.1 ～ 118
[2]	赵自强,丁启秀主编.中南区区域地层[M].武汉:中国地质大学出版社,1996.71～123[Zhao Ziqiang,Ding Qixiu.The regional stratigraphy in central and south part of China[M]. Wuhan: China U-niversity of Geosienes Press,1996 71～123]
[3]	董卫平主编.贵州省岩石地层[M].武汉:中国地质大学出版社,1997. 143 ～ 220 [Dong Weiping. Lithostratigraphy in Guizhou [M].Wuhan: China University of Geosciences Press, 1997. 143～220]
[4]	殷保安主编.广西状族自治区岩石地层[M].武汉:中国地质大学出版社,1997 52～191[Yin Baoan.Lithostratigraphy in Guangxi[M].Wuhan:China University of Geosciences Press,1997.52～191]
[5]	曾允乎,张锦泉,刘文均等.中国南方泥盆纪岩相古地理与成矿作用[M].北京:地质出版社,1994.1～120[Zen Yunfu,Zhang Jinquan, Liu Wenjun, Zhou Huailin, Chen Hongde. Devonian lithofacies paleogeography and mineralization in south China[M]. Beijing: Geological Publishing House, 1994. 1～120]
[6]	吴诒,周怀玲,蒋廷操等.广西泥盆纪沉积相古地理及矿产[M].南宁:广西人民出版社,1987.1～256[Wu Yi,Zhou Huailing,Jiang Tingchao Fang Daonian, Huang Wusheng. The sedimentary facies paleogeography and relatively mineral deposits of Devonian in Guangxi[M].Nanning: Guangxi Peoples Publishing Hoase, 1987.1 ～256]
[7]	钟铿,吴诒,殷保安等.广西的泥盆系[M].武汉:中国地质大学出版社,1992.1～370[Zhong Keng,Wu Yi,YinBaoan,et al.Devonian systen of Guangxi[M]. Wuhan: China University of Geosciences Press, 1992. 1～370]
[8]	邝网敦,赵明特,陶业斌编著广西六景泥盆系剖面[M].武汉:中国地质大学出版社,1989.1～155[Kuang Guodun,Zhao Mingte,Tao Yebin. The standard Devonian section of China: Liujing section of Guangxi[M]. Wuhan: China University of Geosciences Press, 1989.1～154]
[9]	许效松,牟传龙,林明著.露头层序地层与华南泥盆纪古地理[M].成都:成都科技大学出版社,1993.1～288[Xu Xiaosong,Mou Chuanlong, Lin Ming. The outcrop sequence stratigraphy of Devonian and palcogeography in south-China[M]. Chengdu: Chengdu University of Sciencs and Technology Press, 1993. 1 ～288]
[10]	吴诒,龚一鸣,杜远生.华南泥盆纪层序地层及海平面变化[M].武汉:中国地质大学出版社,1997.1～98[Wu Yi,Du Yuansheng,Gong Yiming. Devonian sequenoe stratigraphy and the relative sea-lev-el changes in South-China [M]. Wuban: China University of Geosciences Press, 1997. 1～98]
[11]	杨惠民,刘炳温,邓宗怀等.滇黔桂海相碳酸盐岩地区最佳油气保存单元的评价与选择[M].贵阳:贵州科技出版社,1999.4～63[Yang Huiming, Liu Binwen, Deng Zonghuai, et al. Value and Selection to the Best Gas-Oil Keeping Unite of Marine Carbonate Area in Yunnan, Guizhou and Guangxi[M]. Guiyang: Guizhou Science and Technology Press, 1999. 4 ～63]
[12]	梅冥相,马永生,戴少武等.南盘江盆地晚古生代盆地充填序列特征及生储盖组合划分[J].现代地质,2001,15(1):74～82[Mei Mingxiang, Ma Yongsheng, Dai Shaowu, et al. Late Paleozoic filling succession of the Dianqiangui Basin and the division of association of oilgenerating strata, reservoir, and capping bed[J]. Geosciences,2001,15(1), 74～82]
[13]	吴浩若.广西加里东运动构造古地理问题[J].古地理学报,2000,2(1): 70 ～ 76 [Wu Haoruo. A discussion on the tectonic paleogeography related to the Caledonian movement in Guangxi[J]. Journal of Paleogeography, 2000,2(1): 70～76]
[14]	陈旭,阮亦萍,AJ布科主编,中国古生代气候演变[M].北京:科学出版社,2001 40～53[Chen Xu,Ruan Yiping,A J Boucot.The climate evolution of Plaeozoic in China [M]. Beijing: Sciences Press, 2001, 40～53]
[15]	梅冥相,马永生.从旋回层序的特征论地层记录的两种相变面及两种穿时性[J].地层学杂志,2001,25(2):150～153[Mei Mingxiang, Ma Yongsheng. On two kinds of Facies-change surface and two kinds of diachronisa in stratigraphical records according to the natures of cyclic-sequences[J]. Journal of Stratigraphy, 2001,25(2): 150-153]
[16]	梅冥相.从地层记录的特征论岩石地层学的困惑[J].地层学杂志,1996,20(3):207～212[Mei Mingxiang.On the perplexity of lithostratigraphy according to the natures of stratigraphic records[J].Journal of Stratigraphy, 1996, 20(3): 207～212]
[17]	周希云.贵州泥盆纪几个地层问题的讨论[J].贵州地质,1992,9(4): 331～339[Zhou Xiyun. On discussion of the several problens on Devonian stratigraphy[J]. Guizhou Geology, 1992, 9 (4): 331 ～339]
[18]	Enos P , Wei Jiayong, Lehrmann D J. Death in Guizhou-Late Triassic dromning of the Yangtze carbonate platform[J]. Sedimentary Geology, 1998, 118:55～76
[19]	Johson J G, Klapper G. North American Midcontinent Devonian T-R cycles[J]. Oklahoma Geological Survey Bulletin, 1992,145: 127～135
[20]	Ross C A, Ross J R P. Late Paleozoic transgressive-regressive deposition[A]. In: Wilgus C K, ed. Sea-level Changes: an Integrated Aptoroach[C]. SEPM Spec Pub, 1988, 42:227～247

Devonian Sequence Stratigraphy and Relative Sea-level Changes in Guizhou and Guangxi Area, South China

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