Detrital Composition of Mesozoic Sandstone and Its Implication for Provenance and Tectonic Evolution of Beipiao(Jin-Yang) Basin,Western Liaon ing Province

YAN Yi; LIN Ge; LI Zi-an; HE Shi-jie; XU Zheng-yu

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Article Navigation > Acta Sedimentologica Sinica > 2003 > 21(3): 441-447

YAN Yi, LIN Ge, LI Zi-an, HE Shi-jie, XU Zheng-yu. Detrital Composition of Mesozoic Sandstone and Its Implication for Provenance and Tectonic Evolution of Beipiao(Jin-Yang) Basin,Western Liaon ing Province[J]. Acta Sedimentologica Sinica, 2003, 21(3): 441-447.

Citation:

Detrital Composition of Mesozoic Sandstone and Its Implication for Provenance and Tectonic Evolution of Beipiao(Jin-Yang) Basin,Western Liaon ing Province

1.
Guangzhou Institute of Geochemistry, Chinese Academy of Sci ences, Guangzhou 510640;
2.
Hangzhou Petroleum Institute, Hangzhou 310023

Received Date: 2001-11-19
Rev Recd Date: 2003-01-20
Publish Date: 2003-09-10

Abstract

According to the research on detrital composition of Mesozoic sandstone, it is p roposed that the detrital maturity of the sandstone in Beipiao (Jin-yang) basin is low, and these sandstones contain abundant volcanic lithics,quartz and felds par. Combining basin tectonic setting and sedimentary sequence feature, it can b e deduced that the upper-Triassic sedimentary detritus was eroded from the upli fted regions around the basin. During early Jurassic, Liaoxi area experience d intensely tectonic activation, accompanied by inhomogeneous uplifting, an d Beipiao (Jin-yang) basin subsided and expanded. The Archean basement rocks might have become an important source of the upper Jurassic as a reault of the southeast-trending thrust faulting. In early Cretaceous, the tectonic setting of Liaoxi area changed from squeezing to stretching, and Beipiao (Jinyang) basin ceased evolution. It can also be seen that Dickinson QFL triangle diagram is n ot completely suitable to the western Liaoning province.
- Beipiao( Jin -Yang)basin,
- detrital composition,
- tectonic evolution,
- provenance,

References

[1]	Dickinson W R, Suczek C A. Plate tectonics and sandstone composition[J]. AAPG Bulletin, 1979,63(12): 2164～2182
[2]	Dickinson W R, Valloni R. Provenance of North American Phanerozoic sandstones in relation to tectonic setting[J]. Geological Science of America Bullitin, 1983,94(2): 222～235
[3]	Graham S A, Hendrix M S, Wang L B, et al. Collisional successor basins of western China: Impact of tectonic inheritance on sand composition[J]. Geol Soc Ame Bull, 1993, 105(3): 323～344
[4]	Mack G H. Exceptions to the relationship between plate tectonics and sandstone composition[J]. Journal of Sedimentary Petrology, 1984, 54:21～220
[5]	赵越,杨振宇,马醒华.东亚大地构造发展的重要转折[J]. 地质科学,1994, 29(2): 105～119[ZhaoYue, Yang Zhenyu, Ma Xinghua. Geotectonic transition from paleoasian system and paleotethyan system to paleopacific active continental margin in eastern Asia[J]. Scientia Geologica Sinica, 1994, 29(2): 105～119 ]
[6]	崔盛芹,李锦蓉.试论中国滨太平洋带的印支运动[J].地质学报,1983,1:51～62 [Cui Shengqin, Li Jinrong. On the Indosinian movement of China's peri-pacific tectonic belt[J]. Acta Geological Sinica, 1983, 1:51～62]
[7]	程裕淇.中国区域地质概论[M].北京:地质出版社, 1994[Cheng Yuqi. Outline on regional geology of China[M]. Beijing: Geological Publishing House, 1994]
[8]	陈国达.地洼学说-活化构造及成矿理论体系概论[M].长沙:中南工业大学出版社,1996[Chen Gouda. DIWA theory-outline on activated tectonics and metallogenic theoretic system[M]. Changsha: Central South University of Technology Press, 1996
[9]	邵济安,牟宝磊,张履桥.华北东部中生代构造格局转换过程中的深部作用与浅部响应[J]. 地质论评,2000, 46(1): 32～40[Xiao Jian, Mou Baolei, Zhang Luqiao. Deep geological process and its shallow response during Mesozoic transfer of tectonic frameworks in eastern north China[J]. Geological Review, 2000, 46(1):32～40
[10]	邓晋福,刘厚祥,赵海玲等. 燕辽地区燕山期火成岩与造山模型[J].现代地质,1996,10(2):137～148[ Deng Jinfu, Liu Houxiang, Zhao Hailing, et al. Yanshanian igneous and orogenic model[J]. Geoscience, 1996, 10(2):137～148]
[11]	董树文,吴锡浩,吴珍汉等. 论东亚大陆的构造翘变[J]. 地质论评,2000,46(1): 8～13[Dong Shuwen, Wu Xihao, Wu Zhenhan, et al. On tectonic seesawing of the east continent[J]. Geological Review, 2000, 46(1):8～13]
[12]	张宏仁. 燕山事件[J]. 地质学报,1997,19(8):339～346[Zhang Hongren. Yanshan event [J]. Acta Geological Sinica, 1997,19(8):339～346]
[13]	王根厚,张长厚,王果胜等.辽西地区中生代构造格局及其形成演化[J].现代地质,2001,15(1):1～7[Wang Genhou, Zhang Changhou, Wang Gousheng, et al. Tectonic framework of western Liaoning province and its evolution during Mesozoic[J].Modern Geosciences, 2001, 15(1): 1～7]
[14]	闫义,林舸. 辽西北票盆地侏罗系充填序列及对区域构造演化的指示[J]. 地层学杂志,2002,26(2):151～155[Yan Yi, Lin Ge. Characteristics of the Jurassic filling sequence and the indication of tectonic evolution of Beipiao basin, Western Liaoning province[J]. Journal of Stratigraphy, 2002,26(2):151～155]
[15]	任纪舜,牛宝贵,和政军等. 中国东部的构造格局和演化[J].地学研究,1997,29～30;43～55[Ren Jishun, Nu Baogui, He Zhenjun, et al. The tectonic framwork and development in the eastern China[J]. Geology Research, 1997,29～30: 43～55]
[16]	宋鸿林.燕山式板内造山带基本特征与动力学探讨[J].地学前缘,1999,6(4):309～316[ Song Honglin. Characteristics of Yanshan type intraplate orogenic belts and a discussion on its dynamics[J]. Earth Science Frontiers, 1999, 6(4): 309～316]
[17]	崔盛芹.论全球性中-新生代陆内造山作用与造山带[J]. 地学前缘,1999,6(4):283～293[Cui Shengqin. On global Meso-Cenozoic intracontinental orogenesis and orogenic belts[J]. Earth Science Frontiers, 1999, 6(4):283～293]
[18]	赵温霞.燕山式板内造山作用在北京西山的表现特征及若干启示[J].地质科技情报,2001, 20(2):23～25[Zhao Wenxia. Represented character and several revealations about Yanshan mode interplate orogenesis acting on the west-hill Beijing[J]. Geological Science and Technology Information, 2001, 20(2): 23～25]
[19]	陈国达. 中国地台"活化区"的实例并着重讨论"华夏古陆"问题[J]. 地质学报,1956, 36(3):239～272[Chen Guoda. Examples of "activiting region" in the Chinese platform with special reference to the "cathaysia" problem[J]. Acta Geological Sinica, 1956,36(3): 239～272]
[20]	牟保磊,阎国翰. 燕辽三叠纪碱性偏碱性杂岩体地球化学特征及意义[J].地质学报,1992,66(2):108～120[Mou Baolei, Yan Gouhan. Geochemistry of Triassic alkaline or subalkaline igneous complexes in the Yan-Liao area and their significance[J]. Acta Geological Sinica, 1992, 66(2):108～120]
[21]	和政军,李锦铁,牛宝贵. 燕山-阴山地区晚侏罗世强烈推覆-隆升事件及沉积响应[J].地质论评,1998, 44(4):407～418[He Zhenjun, Li Jintie, Nu Baogui. A preliminary research on sedimentary features and genetic mechanism of frontal basins before Jurassic large-scale nappe in the northern region of north China[J]. Science Geological Sinica, 1998, 44(4):407～418]
[22]	闫义,林舸. 北票盆地中生代砾岩沉积特征及对区域构造演化的指示[J].大地构造与成矿学,2001, 25(4): 15～19[Yan Yi, Lin Ge. The depositional characteristics of Mesozoic conglomerates and the indication to the structural development of Beipiao basin[J]. Geotectonic and Metallogenia, 2001,25(4):15～19]

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通讯作者: 陈斌, bchen63@163.com

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沈阳化工大学材料科学与工程学院沈阳 110142

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Detrital Composition of Mesozoic Sandstone and Its Implication for Provenance and Tectonic Evolution of Beipiao(Jin-Yang) Basin,Western Liaon ing Province

1. Guangzhou Institute of Geochemistry, Chinese Academy of Sci ences, Guangzhou 510640;

2. Hangzhou Petroleum Institute, Hangzhou 310023

Received Date: 2001-11-19

Rev Recd Date: 2003-01-20

Publish Date: 2003-09-10

Key words:

Abstract: According to the research on detrital composition of Mesozoic sandstone, it is p roposed that the detrital maturity of the sandstone in Beipiao (Jin-yang) basin is low, and these sandstones contain abundant volcanic lithics,quartz and felds par. Combining basin tectonic setting and sedimentary sequence feature, it can b e deduced that the upper-Triassic sedimentary detritus was eroded from the upli fted regions around the basin. During early Jurassic, Liaoxi area experience d intensely tectonic activation, accompanied by inhomogeneous uplifting, an d Beipiao (Jin-yang) basin subsided and expanded. The Archean basement rocks might have become an important source of the upper Jurassic as a reault of the southeast-trending thrust faulting. In early Cretaceous, the tectonic setting of Liaoxi area changed from squeezing to stretching, and Beipiao (Jinyang) basin ceased evolution. It can also be seen that Dickinson QFL triangle diagram is n ot completely suitable to the western Liaoning province.

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Reference (22)

[1]	Dickinson W R, Suczek C A. Plate tectonics and sandstone composition[J]. AAPG Bulletin, 1979,63(12): 2164～2182
[2]	Dickinson W R, Valloni R. Provenance of North American Phanerozoic sandstones in relation to tectonic setting[J]. Geological Science of America Bullitin, 1983,94(2): 222～235
[3]	Graham S A, Hendrix M S, Wang L B, et al. Collisional successor basins of western China: Impact of tectonic inheritance on sand composition[J]. Geol Soc Ame Bull, 1993, 105(3): 323～344
[4]	Mack G H. Exceptions to the relationship between plate tectonics and sandstone composition[J]. Journal of Sedimentary Petrology, 1984, 54:21～220
[5]	赵越,杨振宇,马醒华.东亚大地构造发展的重要转折[J]. 地质科学,1994, 29(2): 105～119[ZhaoYue, Yang Zhenyu, Ma Xinghua. Geotectonic transition from paleoasian system and paleotethyan system to paleopacific active continental margin in eastern Asia[J]. Scientia Geologica Sinica, 1994, 29(2): 105～119 ]
[6]	崔盛芹,李锦蓉.试论中国滨太平洋带的印支运动[J].地质学报,1983,1:51～62 [Cui Shengqin, Li Jinrong. On the Indosinian movement of China's peri-pacific tectonic belt[J]. Acta Geological Sinica, 1983, 1:51～62]
[7]	程裕淇.中国区域地质概论[M].北京:地质出版社, 1994[Cheng Yuqi. Outline on regional geology of China[M]. Beijing: Geological Publishing House, 1994]
[8]	陈国达.地洼学说-活化构造及成矿理论体系概论[M].长沙:中南工业大学出版社,1996[Chen Gouda. DIWA theory-outline on activated tectonics and metallogenic theoretic system[M]. Changsha: Central South University of Technology Press, 1996
[9]	邵济安,牟宝磊,张履桥.华北东部中生代构造格局转换过程中的深部作用与浅部响应[J]. 地质论评,2000, 46(1): 32～40[Xiao Jian, Mou Baolei, Zhang Luqiao. Deep geological process and its shallow response during Mesozoic transfer of tectonic frameworks in eastern north China[J]. Geological Review, 2000, 46(1):32～40
[10]	邓晋福,刘厚祥,赵海玲等. 燕辽地区燕山期火成岩与造山模型[J].现代地质,1996,10(2):137～148[ Deng Jinfu, Liu Houxiang, Zhao Hailing, et al. Yanshanian igneous and orogenic model[J]. Geoscience, 1996, 10(2):137～148]
[11]	董树文,吴锡浩,吴珍汉等. 论东亚大陆的构造翘变[J]. 地质论评,2000,46(1): 8～13[Dong Shuwen, Wu Xihao, Wu Zhenhan, et al. On tectonic seesawing of the east continent[J]. Geological Review, 2000, 46(1):8～13]
[12]	张宏仁. 燕山事件[J]. 地质学报,1997,19(8):339～346[Zhang Hongren. Yanshan event [J]. Acta Geological Sinica, 1997,19(8):339～346]
[13]	王根厚,张长厚,王果胜等.辽西地区中生代构造格局及其形成演化[J].现代地质,2001,15(1):1～7[Wang Genhou, Zhang Changhou, Wang Gousheng, et al. Tectonic framework of western Liaoning province and its evolution during Mesozoic[J].Modern Geosciences, 2001, 15(1): 1～7]
[14]	闫义,林舸. 辽西北票盆地侏罗系充填序列及对区域构造演化的指示[J]. 地层学杂志,2002,26(2):151～155[Yan Yi, Lin Ge. Characteristics of the Jurassic filling sequence and the indication of tectonic evolution of Beipiao basin, Western Liaoning province[J]. Journal of Stratigraphy, 2002,26(2):151～155]
[15]	任纪舜,牛宝贵,和政军等. 中国东部的构造格局和演化[J].地学研究,1997,29～30;43～55[Ren Jishun, Nu Baogui, He Zhenjun, et al. The tectonic framwork and development in the eastern China[J]. Geology Research, 1997,29～30: 43～55]
[16]	宋鸿林.燕山式板内造山带基本特征与动力学探讨[J].地学前缘,1999,6(4):309～316[ Song Honglin. Characteristics of Yanshan type intraplate orogenic belts and a discussion on its dynamics[J]. Earth Science Frontiers, 1999, 6(4): 309～316]
[17]	崔盛芹.论全球性中-新生代陆内造山作用与造山带[J]. 地学前缘,1999,6(4):283～293[Cui Shengqin. On global Meso-Cenozoic intracontinental orogenesis and orogenic belts[J]. Earth Science Frontiers, 1999, 6(4):283～293]
[18]	赵温霞.燕山式板内造山作用在北京西山的表现特征及若干启示[J].地质科技情报,2001, 20(2):23～25[Zhao Wenxia. Represented character and several revealations about Yanshan mode interplate orogenesis acting on the west-hill Beijing[J]. Geological Science and Technology Information, 2001, 20(2): 23～25]
[19]	陈国达. 中国地台"活化区"的实例并着重讨论"华夏古陆"问题[J]. 地质学报,1956, 36(3):239～272[Chen Guoda. Examples of "activiting region" in the Chinese platform with special reference to the "cathaysia" problem[J]. Acta Geological Sinica, 1956,36(3): 239～272]
[20]	牟保磊,阎国翰. 燕辽三叠纪碱性偏碱性杂岩体地球化学特征及意义[J].地质学报,1992,66(2):108～120[Mou Baolei, Yan Gouhan. Geochemistry of Triassic alkaline or subalkaline igneous complexes in the Yan-Liao area and their significance[J]. Acta Geological Sinica, 1992, 66(2):108～120]
[21]	和政军,李锦铁,牛宝贵. 燕山-阴山地区晚侏罗世强烈推覆-隆升事件及沉积响应[J].地质论评,1998, 44(4):407～418[He Zhenjun, Li Jintie, Nu Baogui. A preliminary research on sedimentary features and genetic mechanism of frontal basins before Jurassic large-scale nappe in the northern region of north China[J]. Science Geological Sinica, 1998, 44(4):407～418]
[22]	闫义,林舸. 北票盆地中生代砾岩沉积特征及对区域构造演化的指示[J].大地构造与成矿学,2001, 25(4): 15～19[Yan Yi, Lin Ge. The depositional characteristics of Mesozoic conglomerates and the indication to the structural development of Beipiao basin[J]. Geotectonic and Metallogenia, 2001,25(4):15～19]

Detrital Composition of Mesozoic Sandstone and Its Implication for Provenance and Tectonic Evolution of Beipiao(Jin-Yang) Basin,Western Liaon ing Province

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