Characteristics of the Maokou'an Reef in the Zhesiaobao, Inner Mongolia

LI Shang-lin; WANG Xun-lian; XU Xing-yong; ZHANG Hai-jun; LIU Xu-dong; LI Jin-wen

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(3): 434-442

LI Shang-lin, WANG Xun-lian, XU Xing-yong, ZHANG Hai-jun, LIU Xu-dong, LI Jin-wen. Characteristics of the Maokou'an Reef in the Zhesiaobao, Inner Mongolia[J]. Acta Sedimentologica Sinica, 2004, 22(3): 434-442.

Citation:

LI Shang-lin, WANG Xun-lian, XU Xing-yong, ZHANG Hai-jun, LIU Xu-dong, LI Jin-wen. Characteristics of the Maokou'an Reef in the Zhesiaobao, Inner Mongolia[J]. Acta Sedimentologica Sinica, 2004, 22(3): 434-442.

Characteristics of the Maokou'an Reef in the Zhesiaobao, Inner Mongolia

1.
China University of Geosciences, Beijing 100083;
2.
Institute of Marine Geology, Chinese Academy of Sciences, Qingdao Shandong 266071;
3.
Institute of Crustal Dynamics, China Seismological Bureau, Beijing 100085;
4.
Institute of Mineral Resources,Chinese Academy of Geological Sciences, Beijing 100037

Received Date: 2003-06-29
Rev Recd Date: 2003-11-25
Publish Date: 2004-09-10

Abstract

Typical reefs are discovered in the Maokou'an deposits of Zhesiaobo, Inner Mongolia. They extend from east to west, and can be divided into backreef facies, reef front facies and reef core facies clearly. Reef flat, reef crest and reef front margin can be recognized in the reef core facies. The relationship among the various facies suggests that southern part of the reefs are landward, and the northern part seaward. The reefs are very rich in fossils, in which different bioassemblages can be distinguished. The spatial distribution of those assemblages seems to be controlled by facies belts of reefs, and they may exchange laterally from one to anothe.
- reefs,
- Maokou'an Stage,
- Zhesiaobo

References

[1]	Grabau A W. The Permian of Mongolia. Natural History of Central Asia, New York, 1931, 4:1～30
[2]	李良芳.内蒙古达茂旗哲斯敖包早二叠世地层的研究.长春地质学院学报, 1980, 10(3):21～32 [Li Liangfang. Study of the early Permian stratigraphy in Zhesiaobao, Inner Mongolia. Journal of Changchun College of Geology, 1980, 10(3):21～32]
[3]	丁蕴杰,夏国英,段乘华,等.内蒙古哲斯地区早二叠世地层及动物群.中国地质科学院天津地质矿产研究所所刊, 1985,第10号:1～244 [Ding Yunjie, Xia Guoying, Duan Changhua, et al. Study on the early Permian stratigraphy and fauna in Zhesiaobao, Inner Mongolia. Bulletin Tianjin Institute Geol. Min. Res., 1985, (10):1～244]
[4]	内蒙古自治区地质矿产局.内蒙古自治区区域地质志.北京:地质出版社,1991. 202～205 [Bureau of Geology and Mineral Resources of Inner Mongolia. Regional Geology Of Inner Mongolia. Beijing: Geological Publishing House, 1991. 202～205]
[5]	内蒙古自治区地质矿产局.内蒙古自治区岩石地层.武汉:中国地质大学出版社, 1996.107～109,233～239 [Bureau of Geology and Mineral Resources of Inner Mongolia. Stratigraphy (lithostratic) of Inner Mongolia. Wuhan: China University of Geosciences Press, 1996.107～109,233～239]
[6]	Э.Я.Левен,T.A.Грунт,林英铴,等.中国内蒙古哲斯-洪格尔剖面与东欧和特提斯层型区二叠纪沉积对比的意义.世界地质,1998,17(4):9～10 [Э.Я.Левен,T.A.Грунт,Lin Yingdang, et al. Correlation implication for the Permian sediments between Zhesi-Honggeer section in Inner Mongolia,China and stratotype in Easterm and Tethys. Global Geology, 1998, 17(4): 9～10 ]
[7]	刘鹏举,郭伟.内蒙古哲斯地区早二叠世地层的新认识.世界地质,1998,17(2):1～5 [Liu Pengju and Guo Wei . New recognition on Lower Permian in Zhesi, Inner Mongolia. Global Geology, 1998, 17(2): 1～5]
[8]	王惠,陈志勇,杨万容.内蒙古满都拉二叠纪海绵生物丘的发现及意义.地层学杂志,2002,26(1):33～38 [Wang Hui, Chen Zhiyong, and Yang wan rong. Discovery of the Permian sponge mounds in Mandula, Inner Mongolia. Journal of Stratigraphy, 2002, 26(1): 33～38]
[9]	Dunham G R. Classification of carbonate rocks according to depositional texture. AAPG Memior, 1962, 1: 108～121
[10]	Folk R L. Sepectral subdivision of limestones types. AAPG Memior, 1962, 1: 62～84
[11]	Embr A, Klovan J E. A late Devonian reef tract on northeastern Banks Island, Northwest Territories. Bulletin of Canadian Pelagic Geology, 1971, 19: 730～781
[12]	邓占球.广西来宾合山上二叠统海绵化石.古生物学报,1981,20(5):418～420 [Deng Zhanqiu. Upper Permian sponges from laibin of Guanxi. Acta Palaeontologlca Sinica, 1981,20(5):418～420]
[13]	邓占球.记述几种海绵和水螅.古生物学报,1982,21(6):709～713 [Deng Zhanqiu. Note on some sponges and hydroids. Acta Palaeontologlca Sinica, 1982,21(6):709～713]
[14]	杨万容,李讯.中国南方二叠纪礁类型及成礁的控制因素.古生物学报,1995,34(1):67～75 [Yang Wanrong and Li Xun. Permian reef types and controlling factors of reef formtion in south China. Journal of Stratigraphy, 1995,34(1):67～75]
[15]	杨万容,杨长庚,李讯,张国方.浙江桐庐二叠纪海绵生物丘的沉积环境及成岩环境.地层学杂志,1995,19(3):191～197 [Yang Wanrong, Yang chang qing, Li Xun, Zhang Guofang. The sedimentary and diagenesis environments of Permian sponge mound inTonglu, Zhejiang. Journal of Stratigraphy, 1995,19(3):191～197]
[16]	周建平,张遴信,王玉净,杨群.中国二叠纪类生物地理分区.地层学杂志,2000,24(增刊):378～381 [Zhou Jianping, Zhang Linxin, Wang Yujing, Yangqun. Permian biogeography provinces of fusulinids in China. Journal of Stratigraphy, 2000,(Supplement): 378-381]
[17]	贾振远,李之琪.碳酸岩沉积相和沉积环境.武汉:中国地质大学出版社,1989.84～103 [Jia Zhenyuan and Li Zhiqi. Carbonate sedimentary facies and environments. Wuhan: China University of Geosciences Press, 1989.84～103]
[18]	何卫红,王啸风,卜建军.晚奥陶世五峰期扬子海盆地海平面变化旋回与古水深度.沉积学报,2002,20(3):367～371 [He Weihong, Wang Xiaofeng and Bu Jianjun. The eustatic cycles and the depth of water mass of the latest Ordovician Wufengian in the Yangtse Basin. Acta Sedimentologica Sinica, 2002,20(3):367～371]
[19]	李双应,岳双仓.安徽巢湖二叠系栖霞组碳酸盐岩斜坡沉积.沉积学报,2002,20(1):7～12 [Li Shuangying and Yue Shucang. Sedimentation on a carbonate slope of Permian Qixia Formation in Chaohu Region, Anhui. Acta Sedimentologica Sinica, 2002,20(1): 7～12]
[20]	王兴志,张帆,马青,等.四川盆地东部晚二叠世-早三叠世飞仙关期礁、滩特征与海平面变化..沉积学报,2002,20(2):249～254 [Wang Xingzhi, Zhang Fan, Ma Qing, et al. The characteristics of reef and bank and the fluctuation of sea-level in Feixianguan Period of late Permian～early Triassic, east Sichuan Basin. Acta Sedimentologica Sinica, 2002,20(2):249～254]

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Characteristics of the Maokou'an Reef in the Zhesiaobao, Inner Mongolia

1. China University of Geosciences, Beijing 100083;

2. Institute of Marine Geology, Chinese Academy of Sciences, Qingdao Shandong 266071;

3. Institute of Crustal Dynamics, China Seismological Bureau, Beijing 100085;

4. Institute of Mineral Resources,Chinese Academy of Geological Sciences, Beijing 100037

Received Date: 2003-06-29

Rev Recd Date: 2003-11-25

Publish Date: 2004-09-10

Key words:

reefs /
Maokou'an Stage /
Zhesiaobo

Abstract: Typical reefs are discovered in the Maokou'an deposits of Zhesiaobo, Inner Mongolia. They extend from east to west, and can be divided into backreef facies, reef front facies and reef core facies clearly. Reef flat, reef crest and reef front margin can be recognized in the reef core facies. The relationship among the various facies suggests that southern part of the reefs are landward, and the northern part seaward. The reefs are very rich in fossils, in which different bioassemblages can be distinguished. The spatial distribution of those assemblages seems to be controlled by facies belts of reefs, and they may exchange laterally from one to anothe.

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Reference (20)

[1]	Grabau A W. The Permian of Mongolia. Natural History of Central Asia, New York, 1931, 4:1～30
[2]	李良芳.内蒙古达茂旗哲斯敖包早二叠世地层的研究.长春地质学院学报, 1980, 10(3):21～32 [Li Liangfang. Study of the early Permian stratigraphy in Zhesiaobao, Inner Mongolia. Journal of Changchun College of Geology, 1980, 10(3):21～32]
[3]	丁蕴杰,夏国英,段乘华,等.内蒙古哲斯地区早二叠世地层及动物群.中国地质科学院天津地质矿产研究所所刊, 1985,第10号:1～244 [Ding Yunjie, Xia Guoying, Duan Changhua, et al. Study on the early Permian stratigraphy and fauna in Zhesiaobao, Inner Mongolia. Bulletin Tianjin Institute Geol. Min. Res., 1985, (10):1～244]
[4]	内蒙古自治区地质矿产局.内蒙古自治区区域地质志.北京:地质出版社,1991. 202～205 [Bureau of Geology and Mineral Resources of Inner Mongolia. Regional Geology Of Inner Mongolia. Beijing: Geological Publishing House, 1991. 202～205]
[5]	内蒙古自治区地质矿产局.内蒙古自治区岩石地层.武汉:中国地质大学出版社, 1996.107～109,233～239 [Bureau of Geology and Mineral Resources of Inner Mongolia. Stratigraphy (lithostratic) of Inner Mongolia. Wuhan: China University of Geosciences Press, 1996.107～109,233～239]
[6]	Э.Я.Левен,T.A.Грунт,林英铴,等.中国内蒙古哲斯-洪格尔剖面与东欧和特提斯层型区二叠纪沉积对比的意义.世界地质,1998,17(4):9～10 [Э.Я.Левен,T.A.Грунт,Lin Yingdang, et al. Correlation implication for the Permian sediments between Zhesi-Honggeer section in Inner Mongolia,China and stratotype in Easterm and Tethys. Global Geology, 1998, 17(4): 9～10 ]
[7]	刘鹏举,郭伟.内蒙古哲斯地区早二叠世地层的新认识.世界地质,1998,17(2):1～5 [Liu Pengju and Guo Wei . New recognition on Lower Permian in Zhesi, Inner Mongolia. Global Geology, 1998, 17(2): 1～5]
[8]	王惠,陈志勇,杨万容.内蒙古满都拉二叠纪海绵生物丘的发现及意义.地层学杂志,2002,26(1):33～38 [Wang Hui, Chen Zhiyong, and Yang wan rong. Discovery of the Permian sponge mounds in Mandula, Inner Mongolia. Journal of Stratigraphy, 2002, 26(1): 33～38]
[9]	Dunham G R. Classification of carbonate rocks according to depositional texture. AAPG Memior, 1962, 1: 108～121
[10]	Folk R L. Sepectral subdivision of limestones types. AAPG Memior, 1962, 1: 62～84
[11]	Embr A, Klovan J E. A late Devonian reef tract on northeastern Banks Island, Northwest Territories. Bulletin of Canadian Pelagic Geology, 1971, 19: 730～781
[12]	邓占球.广西来宾合山上二叠统海绵化石.古生物学报,1981,20(5):418～420 [Deng Zhanqiu. Upper Permian sponges from laibin of Guanxi. Acta Palaeontologlca Sinica, 1981,20(5):418～420]
[13]	邓占球.记述几种海绵和水螅.古生物学报,1982,21(6):709～713 [Deng Zhanqiu. Note on some sponges and hydroids. Acta Palaeontologlca Sinica, 1982,21(6):709～713]
[14]	杨万容,李讯.中国南方二叠纪礁类型及成礁的控制因素.古生物学报,1995,34(1):67～75 [Yang Wanrong and Li Xun. Permian reef types and controlling factors of reef formtion in south China. Journal of Stratigraphy, 1995,34(1):67～75]
[15]	杨万容,杨长庚,李讯,张国方.浙江桐庐二叠纪海绵生物丘的沉积环境及成岩环境.地层学杂志,1995,19(3):191～197 [Yang Wanrong, Yang chang qing, Li Xun, Zhang Guofang. The sedimentary and diagenesis environments of Permian sponge mound inTonglu, Zhejiang. Journal of Stratigraphy, 1995,19(3):191～197]
[16]	周建平,张遴信,王玉净,杨群.中国二叠纪类生物地理分区.地层学杂志,2000,24(增刊):378～381 [Zhou Jianping, Zhang Linxin, Wang Yujing, Yangqun. Permian biogeography provinces of fusulinids in China. Journal of Stratigraphy, 2000,(Supplement): 378-381]
[17]	贾振远,李之琪.碳酸岩沉积相和沉积环境.武汉:中国地质大学出版社,1989.84～103 [Jia Zhenyuan and Li Zhiqi. Carbonate sedimentary facies and environments. Wuhan: China University of Geosciences Press, 1989.84～103]
[18]	何卫红,王啸风,卜建军.晚奥陶世五峰期扬子海盆地海平面变化旋回与古水深度.沉积学报,2002,20(3):367～371 [He Weihong, Wang Xiaofeng and Bu Jianjun. The eustatic cycles and the depth of water mass of the latest Ordovician Wufengian in the Yangtse Basin. Acta Sedimentologica Sinica, 2002,20(3):367～371]
[19]	李双应,岳双仓.安徽巢湖二叠系栖霞组碳酸盐岩斜坡沉积.沉积学报,2002,20(1):7～12 [Li Shuangying and Yue Shucang. Sedimentation on a carbonate slope of Permian Qixia Formation in Chaohu Region, Anhui. Acta Sedimentologica Sinica, 2002,20(1): 7～12]
[20]	王兴志,张帆,马青,等.四川盆地东部晚二叠世-早三叠世飞仙关期礁、滩特征与海平面变化..沉积学报,2002,20(2):249～254 [Wang Xingzhi, Zhang Fan, Ma Qing, et al. The characteristics of reef and bank and the fluctuation of sea-level in Feixianguan Period of late Permian～early Triassic, east Sichuan Basin. Acta Sedimentologica Sinica, 2002,20(2):249～254]

Characteristics of the Maokou'an Reef in the Zhesiaobao, Inner Mongolia

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