鲕粒粒度特征及其指示意义

郭芪恒; 金振奎; 史书婷; 朱小二; 李硕; 陈媛; 王金艺; 郭芪恒; 金振奎; 史书婷; 朱小二; 李硕; 陈媛; 王金艺

doi:10.14027/j.issn.1000-0550.2019.050

[1]

朱筱敏. 沉积岩石学[M]. 4版. 北京：石油工业出版社，2008.

Zhu Xiaomin. Sedimentary petrology[M]. 4th ed. Beijing: Petroleum Industry Press, 2008.

[2]

郑浚茂，王德发，孙永传. 黄骅拗陷几种砂体的粒度分布特征及其水动力条件的初步分析[J]. 石油实验地质，1980，2（2）：9-20.

Zheng Junmao, Wang Defa, Sun Yongchuan. Preliminary Analysis of particle size distribution characteristics and hydrodynamic conditions of several sand body in Huanghua Depression[J]. Petroleum Geology & Experiment, 1980, 2(2): 9-20.

[3]

雷国良，张虎才，张文翔，等. 柴达木盆地察尔汗古湖贝壳堤剖面粒度特征及其沉积环境[J]. 沉积学报，2007，25（2）：274-282.

Lei Guoliang, Zhang Hucai, Zhang Wenxiang, et al. Characteristics of grain-size and sedimentation of shell bar section in salt lake Qarhan, Qaidam Basin[J]. Acta Sedimentologica Sinica, 2007, 25(2): 274-282.

[4]

董延钰，金芳，黄俊华. 鄱阳湖沉积物粒度特征及其对形成演变过程的示踪意义[J]. 地质科技情报，2011，30（2）：57-62.

Dong Yanyu, Jin Fang, Huang Junhua. Poyang Lake sediments grain size characteristics and its tracing implication for formation and evolution processes[J]. Geological Science and Technology Information, 2011, 30(2): 57-62.

[5]

马龙，吴敬禄，温军会，等. 乌梁素海湖泊沉积物粒度特征及其环境指示意义[J]. 沉积学报，2013，31（4）：646-652.

Ma Long, Wu Jinglu, Wen Junhui, et al. Grain size characteristics and its environmental significance of lacustrine sediment recorded in Wuliangsu Lake, Inner Mongolia[J]. Acta Sedimentologica Sinica, 2013, 31(4): 646-652.

[6]

蒋庆丰，刘兴起，沈吉. 乌伦古湖沉积物粒度特征及其古气候环境意义[J]. 沉积学报，2006，24（6）：877-882.

Jiang Qingfeng, Liu Xingqi, Shen Ji. Grain-size characteristics of Wulugu Lake sediments and its palaeoclimate and palaeoenvironment implication[J]. Acta Sedimentologica Sinica, 2006, 24(6): 877-882.

[7]

朱锐，张昌民，龚福华，等. 粒度资料的沉积动力学在沉积环境分析中的应用：以江汉盆地西北缘上白垩统红花套组沉积为例[J]. 高校地质学报，2010，16（3）：358-364.

Zhu Rui, Zhang Changmin, Gong Fuhua, et al. Use of sediment dynamic analysis in environment interpretation: A case study on Honghuatao Formation, Upper Cretaceous of western Jianghan Basin, Hubei province[J]. Geological Journal of China Universities, 2010, 16(3): 358-364.

[8]

葛东升，刘玉明，柳雪青，等. 粒度分析在致密砂岩储层及沉积环境评价中的应用[J]. 特种油气藏，2018，25（1）：41-45，72.

Ge Dongsheng, Liu Yuming, Liu Xueqing, et al. Application of grain size analysis in tight sandstone reservoir and sedimentary environment evaluation[J]. Special Oil & Gas Reservoirs, 2018, 25(1): 41-45, 72.

[9]

Sumner D Y, Grotzinger J P. Numerical modeling of ooid size and the problem of Neoproterozoic giant ooids[J]. Journal of Sedimentary Petrology, 1993, 63(5): 974-982.

[10]

Trower E J, Lamb M P, Fischer W W. Experimental evidence that ooid size reflects a dynamic equilibrium between rapid precipitation and abrasion rates[J]. Earth and Planetary Science Letters, 2017, 468: 112-118.

[11]

Bathurst R G C. Carbonate sediments and their diagenesis[M]. Amsterdam: Elsevier, 1972: 658.

[12]

Swett K, Knoll A H. Marine Pisolites from Upper Proterozoic carbonates of east Greenland and Spitsbergen[J]. Sedimentology, 1989, 36(1): 75-93.

[13]

赵东方，胡广，张文济，等. 渝北巫溪鱼鳞剖面灯影组鲕粒沉积特征及其地质意义[J]. 地质论评，2018，64（1）：191-202.

Zhao Dongfang, Hu Guang, Zhang Wenji, et al. Sedimentary characteristics of ooids of Sinian (Ediacaran) Dengying Formation on the Yulin section in Wuxi, Chongqing, and geological implications[J]. Geological Review, 2018, 64(1): 191-202.

[14]

付坤荣，黄理力，祝怡，等. 塔中地区晚奥陶世碳酸盐台缘与台内沉积差异：定性和定量的碳酸盐岩微相综合分析[J]. 沉积学报，2018，36（1）：101-109.

Fu Kunrong, Huang Lili, Zhu Yi, et al. The depositional diversity between platform margin and platform interior on the Late Ordovician carbonate rimmed-platform of Tazhong area: A case study of qualitative and quantitative integrated microfacies analysis[J]. Acta Sedimentologica Sinica, 2018, 36(1): 101-109.

[15]

周肖贝，李江海，王洪浩，等. 寒武纪全球板块构造与古地理环境再造[J]. 海相油气地质，2014，19（2）：1-7.

Zhou Xiaobei, Li Jianghai, Wang Honghao, et al. Reconstruction of Cambrian global paleo-plates and paleogeography[J]. Marine Origin Petroleum Geology, 2014, 19(2): 1-7.

[16]

段吉业，刘鹏举，夏德馨. 浅析华北板块中元古代—古生代构造格局及其演化[J]. 现代地质，2002，16（4）：331-338.

Duan Jiye, Liu Pengju, Xia Dexin. The preliminary research on tectonic pattern and tectonic evolution of Mesoproterozoic-Paleozoic in North China Plate[J]. Geoscience, 2002, 16(4): 331-338.

[17]

冯增昭，陈继新，吴胜和. 华北地台早古生代岩相古地理[J]. 沉积学报，1989，7（4）：15-55.

Feng Zengzhao, Chen Jixin, Wu Shenghe. Early Paleozoic lithofacies palaeogeography of the North China Platform[J]. Acta Sedimentologica Sinica, 1989, 7(4): 15-55.

[18]

马永生，梅冥相，周润轩，等. 层序地层框架下的鲕粒滩形成样式：以北京西郊下苇甸剖面寒武系第三统为例[J]. 岩石学报，2017，33（4）：1021-1036.

Ma Yongsheng, Mei Mingxiang, Zhou Runxuan, et al. Forming patterns for the oolitic bank within the sequence-stratigraphic framework: An example from the Cambrian Series 3 at the Xiaweidian section in the western suburb of Beijing[J]. Acta Petrologica Sinica, 2017, 33(4): 1021-1036.

[19]

郭芪恒，金振奎，朱小二，等. 北京下苇甸剖面张夏组鲕粒特征及其白云化机制[J]. 现代地质，2018，32（4）：766-773.

Guo Qiheng, Jin Zhenkui, Zhu Xiaoer, et al. Characteristics of oolites and their dolomitization mechanism of the Cambrian Zhangxia Formation at Xiaweidian outcrop in Beijing[J]. Geoscience, 2018, 32(4): 766-773.

[20]

北京市地质矿产局. 北京市区域地质志[M]. 北京：地质出版社，1991.

Beijing Bureau of Geology and Mineral Resources. People's republic of China ministry of geology and mineral resources[M]. Beijing: Geological Publishing House, 1991.

[21]

郭芪恒，金振奎，安益辰，等. 北京下苇甸地区张夏组沉积环境及沉积模式[J]. 沉积学报，2019，37（1）：40-50.

Guo Qiheng, Jin Zhenkui, An Yichen, et al. Study on sedimentary environment and patterns of the Cambrian Zhangxia Formation at Xiaweidian, Beijing[J]. Acta Sedimentologica Sinica, 2019, 37(1): 40-50.

[22]

Friedman G M. Comparison of moment measures for sieving and thin-section data in sedimentary petrological studies[J]. Journal of sedimentary Research, 1962, 32(1): 15-25.

[23]

Folk R L, Ward W C. Brazos river bar: A study in the significance of grain size parameters[J]. Journal of sedimentary Petrology, 1957, 27(1): 3-26.

[24]

陈俊飞，李琦，朱如凯，等. 鄂尔多斯盆地西南部长8段致密砂岩储层粒度特征及其环境指示意义[J]. 大庆石油地质与开发，2018，37（4）：10-19.

Chen Junfei, Li Qi, Zhu Rukai, et al. Grain-size characteristics of the tight sandstone reservoir and their environmental indicating significances for member Chang-8 in Southwest Ordos Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2018, 37(4): 10-19.

[25]

Davies P J, Bubela B, Ferguson J. The formation of ooids[J]. Sedimentology, 1978, 25(5): 703-730.

[26]

Diaz M R, Eberli G P, Blackwelder P, et al. Microbially mediated organomineralization in the formation of ooids[J]. Geology, 2017, 45(9): 771-774.

[27]

Summons R E, Bird L R, Gillespie A L, et al. Lipid biomarkers in ooids from different locations and ages: Evidence for a common bacterial flora[J]. Geobiology, 2013, 11(5): 420-436.

[28]

梅冥相，马永生，梅仕龙，等. 华北寒武系层序地层格架及碳酸盐台地演化[J]. 现代地质，1997，11（3）：275-282.

Mei Ming⁃xiang, Ma Yongsheng, Mei Shilong, et al. Framwork of Cambrian sedimentary sequence and evolution of carbonate platform in North China[J]. Geoscience, 1997, 11(3): 275-282.

[29]

刘波，钱祥麟，王英华. 华北板块早古生代构造—沉积演化[J]. 地质科学，1999，34（3）：347-356.

Liu Bo, Qian Xianglin, Wang Yinghua. Tectono-sedimentary evolution of North China Plate in Early Paleozoic[J]. Scientia Geologica Sinica, 1999, 34(3): 347-356.

[30]

金振奎，邵冠铭. 石灰岩分类新方案[J]. 新疆石油地质，2014，35（2）：235-242.

Jin Zhenkui, Shao Guanming. New classification scheme of limestones[J]. Xinjiang Petroleum Geology, 2014, 35(2): 235-242.

[31]

Sandberg P A. New interpretations of Great Salt Lake ooids and of ancient non-skeletal carbonate mineralogy[J]. Sedimentology, 1975, 22(4): 497-537.

[32]

Siahi M, Hofmann A, Master S, et al. Carbonate ooids of the mesoarchaean Pongola supergroup, South Africa[J]. Geobiology, 2017, 15(6): 750-766.

[33]

Duguid S M A, Kyser T K, James N P, et al. Microbes and ooids[J]. Journal of Sedimentary Research, 2010, 80(3): 236-251.

[34]

解艳玲，庄军. 鄂尔多斯盆地南部延安组砂体粒度特征[J]. 中国矿业大学学报，1998，27（4）：428-432.

Xie Yanling, Zhuang Jun. Particle size and depositional environment of sandstone of Yan’an Formation in South Ordos Basin[J]. Journal of China University of Mining & Technology, 1998, 27(4): 428-432.

[35]

袁文芳，陈世悦，曾昌民，等. 柴达木盆地西部地区第三系碎屑岩粒度概率累积曲线特征[J]. 石油大学学报（自然科学版），2005，29（5）：12-18.

Yuan Wenfang, Chen Shiyue, Zeng Changmin, et al. Probability cumulative grain size curves in terrigenous of the Tertiary in west Qaidam Basin[J]. Journal of the University of Petroleum, China, 2005, 29(5): 12-18.

[1]	朱筱敏. 沉积岩石学[M]. 4版. 北京：石油工业出版社，2008. Zhu Xiaomin. Sedimentary petrology[M]. 4th ed. Beijing: Petroleum Industry Press, 2008.
[2]	郑浚茂，王德发，孙永传. 黄骅拗陷几种砂体的粒度分布特征及其水动力条件的初步分析[J]. 石油实验地质，1980，2（2）：9-20. Zheng Junmao, Wang Defa, Sun Yongchuan. Preliminary Analysis of particle size distribution characteristics and hydrodynamic conditions of several sand body in Huanghua Depression[J]. Petroleum Geology & Experiment, 1980, 2(2): 9-20.
[3]	雷国良，张虎才，张文翔，等. 柴达木盆地察尔汗古湖贝壳堤剖面粒度特征及其沉积环境[J]. 沉积学报，2007，25（2）：274-282. Lei Guoliang, Zhang Hucai, Zhang Wenxiang, et al. Characteristics of grain-size and sedimentation of shell bar section in salt lake Qarhan, Qaidam Basin[J]. Acta Sedimentologica Sinica, 2007, 25(2): 274-282.
[4]	董延钰，金芳，黄俊华. 鄱阳湖沉积物粒度特征及其对形成演变过程的示踪意义[J]. 地质科技情报，2011，30（2）：57-62. Dong Yanyu, Jin Fang, Huang Junhua. Poyang Lake sediments grain size characteristics and its tracing implication for formation and evolution processes[J]. Geological Science and Technology Information, 2011, 30(2): 57-62.
[5]	马龙，吴敬禄，温军会，等. 乌梁素海湖泊沉积物粒度特征及其环境指示意义[J]. 沉积学报，2013，31（4）：646-652. Ma Long, Wu Jinglu, Wen Junhui, et al. Grain size characteristics and its environmental significance of lacustrine sediment recorded in Wuliangsu Lake, Inner Mongolia[J]. Acta Sedimentologica Sinica, 2013, 31(4): 646-652.
[6]	蒋庆丰，刘兴起，沈吉. 乌伦古湖沉积物粒度特征及其古气候环境意义[J]. 沉积学报，2006，24（6）：877-882. Jiang Qingfeng, Liu Xingqi, Shen Ji. Grain-size characteristics of Wulugu Lake sediments and its palaeoclimate and palaeoenvironment implication[J]. Acta Sedimentologica Sinica, 2006, 24(6): 877-882.
[7]	朱锐，张昌民，龚福华，等. 粒度资料的沉积动力学在沉积环境分析中的应用：以江汉盆地西北缘上白垩统红花套组沉积为例[J]. 高校地质学报，2010，16（3）：358-364. Zhu Rui, Zhang Changmin, Gong Fuhua, et al. Use of sediment dynamic analysis in environment interpretation: A case study on Honghuatao Formation, Upper Cretaceous of western Jianghan Basin, Hubei province[J]. Geological Journal of China Universities, 2010, 16(3): 358-364.
[8]	葛东升，刘玉明，柳雪青，等. 粒度分析在致密砂岩储层及沉积环境评价中的应用[J]. 特种油气藏，2018，25（1）：41-45，72. Ge Dongsheng, Liu Yuming, Liu Xueqing, et al. Application of grain size analysis in tight sandstone reservoir and sedimentary environment evaluation[J]. Special Oil & Gas Reservoirs, 2018, 25(1): 41-45, 72.
[9]	Sumner D Y, Grotzinger J P. Numerical modeling of ooid size and the problem of Neoproterozoic giant ooids[J]. Journal of Sedimentary Petrology, 1993, 63(5): 974-982.
[10]	Trower E J, Lamb M P, Fischer W W. Experimental evidence that ooid size reflects a dynamic equilibrium between rapid precipitation and abrasion rates[J]. Earth and Planetary Science Letters, 2017, 468: 112-118.
[11]	Bathurst R G C. Carbonate sediments and their diagenesis[M]. Amsterdam: Elsevier, 1972: 658.
[12]	Swett K, Knoll A H. Marine Pisolites from Upper Proterozoic carbonates of east Greenland and Spitsbergen[J]. Sedimentology, 1989, 36(1): 75-93.
[13]	赵东方，胡广，张文济，等. 渝北巫溪鱼鳞剖面灯影组鲕粒沉积特征及其地质意义[J]. 地质论评，2018，64（1）：191-202. Zhao Dongfang, Hu Guang, Zhang Wenji, et al. Sedimentary characteristics of ooids of Sinian (Ediacaran) Dengying Formation on the Yulin section in Wuxi, Chongqing, and geological implications[J]. Geological Review, 2018, 64(1): 191-202.
[14]	付坤荣，黄理力，祝怡，等. 塔中地区晚奥陶世碳酸盐台缘与台内沉积差异：定性和定量的碳酸盐岩微相综合分析[J]. 沉积学报，2018，36（1）：101-109. Fu Kunrong, Huang Lili, Zhu Yi, et al. The depositional diversity between platform margin and platform interior on the Late Ordovician carbonate rimmed-platform of Tazhong area: A case study of qualitative and quantitative integrated microfacies analysis[J]. Acta Sedimentologica Sinica, 2018, 36(1): 101-109.
[15]	周肖贝，李江海，王洪浩，等. 寒武纪全球板块构造与古地理环境再造[J]. 海相油气地质，2014，19（2）：1-7. Zhou Xiaobei, Li Jianghai, Wang Honghao, et al. Reconstruction of Cambrian global paleo-plates and paleogeography[J]. Marine Origin Petroleum Geology, 2014, 19(2): 1-7.
[16]	段吉业，刘鹏举，夏德馨. 浅析华北板块中元古代—古生代构造格局及其演化[J]. 现代地质，2002，16（4）：331-338. Duan Jiye, Liu Pengju, Xia Dexin. The preliminary research on tectonic pattern and tectonic evolution of Mesoproterozoic-Paleozoic in North China Plate[J]. Geoscience, 2002, 16(4): 331-338.
[17]	冯增昭，陈继新，吴胜和. 华北地台早古生代岩相古地理[J]. 沉积学报，1989，7（4）：15-55. Feng Zengzhao, Chen Jixin, Wu Shenghe. Early Paleozoic lithofacies palaeogeography of the North China Platform[J]. Acta Sedimentologica Sinica, 1989, 7(4): 15-55.
[18]	马永生，梅冥相，周润轩，等. 层序地层框架下的鲕粒滩形成样式：以北京西郊下苇甸剖面寒武系第三统为例[J]. 岩石学报，2017，33（4）：1021-1036. Ma Yongsheng, Mei Mingxiang, Zhou Runxuan, et al. Forming patterns for the oolitic bank within the sequence-stratigraphic framework: An example from the Cambrian Series 3 at the Xiaweidian section in the western suburb of Beijing[J]. Acta Petrologica Sinica, 2017, 33(4): 1021-1036.
[19]	郭芪恒，金振奎，朱小二，等. 北京下苇甸剖面张夏组鲕粒特征及其白云化机制[J]. 现代地质，2018，32（4）：766-773. Guo Qiheng, Jin Zhenkui, Zhu Xiaoer, et al. Characteristics of oolites and their dolomitization mechanism of the Cambrian Zhangxia Formation at Xiaweidian outcrop in Beijing[J]. Geoscience, 2018, 32(4): 766-773.
[20]	北京市地质矿产局. 北京市区域地质志[M]. 北京：地质出版社，1991. Beijing Bureau of Geology and Mineral Resources. People's republic of China ministry of geology and mineral resources[M]. Beijing: Geological Publishing House, 1991.
[21]	郭芪恒，金振奎，安益辰，等. 北京下苇甸地区张夏组沉积环境及沉积模式[J]. 沉积学报，2019，37（1）：40-50. Guo Qiheng, Jin Zhenkui, An Yichen, et al. Study on sedimentary environment and patterns of the Cambrian Zhangxia Formation at Xiaweidian, Beijing[J]. Acta Sedimentologica Sinica, 2019, 37(1): 40-50.
[22]	Friedman G M. Comparison of moment measures for sieving and thin-section data in sedimentary petrological studies[J]. Journal of sedimentary Research, 1962, 32(1): 15-25.
[23]	Folk R L, Ward W C. Brazos river bar: A study in the significance of grain size parameters[J]. Journal of sedimentary Petrology, 1957, 27(1): 3-26.
[24]	陈俊飞，李琦，朱如凯，等. 鄂尔多斯盆地西南部长8段致密砂岩储层粒度特征及其环境指示意义[J]. 大庆石油地质与开发，2018，37（4）：10-19. Chen Junfei, Li Qi, Zhu Rukai, et al. Grain-size characteristics of the tight sandstone reservoir and their environmental indicating significances for member Chang-8 in Southwest Ordos Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2018, 37(4): 10-19.
[25]	Davies P J, Bubela B, Ferguson J. The formation of ooids[J]. Sedimentology, 1978, 25(5): 703-730.
[26]	Diaz M R, Eberli G P, Blackwelder P, et al. Microbially mediated organomineralization in the formation of ooids[J]. Geology, 2017, 45(9): 771-774.
[27]	Summons R E, Bird L R, Gillespie A L, et al. Lipid biomarkers in ooids from different locations and ages: Evidence for a common bacterial flora[J]. Geobiology, 2013, 11(5): 420-436.
[28]	梅冥相，马永生，梅仕龙，等. 华北寒武系层序地层格架及碳酸盐台地演化[J]. 现代地质，1997，11（3）：275-282. Mei Ming⁃xiang, Ma Yongsheng, Mei Shilong, et al. Framwork of Cambrian sedimentary sequence and evolution of carbonate platform in North China[J]. Geoscience, 1997, 11(3): 275-282.
[29]	刘波，钱祥麟，王英华. 华北板块早古生代构造—沉积演化[J]. 地质科学，1999，34（3）：347-356. Liu Bo, Qian Xianglin, Wang Yinghua. Tectono-sedimentary evolution of North China Plate in Early Paleozoic[J]. Scientia Geologica Sinica, 1999, 34(3): 347-356.
[30]	金振奎，邵冠铭. 石灰岩分类新方案[J]. 新疆石油地质，2014，35（2）：235-242. Jin Zhenkui, Shao Guanming. New classification scheme of limestones[J]. Xinjiang Petroleum Geology, 2014, 35(2): 235-242.
[31]	Sandberg P A. New interpretations of Great Salt Lake ooids and of ancient non-skeletal carbonate mineralogy[J]. Sedimentology, 1975, 22(4): 497-537.
[32]	Siahi M, Hofmann A, Master S, et al. Carbonate ooids of the mesoarchaean Pongola supergroup, South Africa[J]. Geobiology, 2017, 15(6): 750-766.
[33]	Duguid S M A, Kyser T K, James N P, et al. Microbes and ooids[J]. Journal of Sedimentary Research, 2010, 80(3): 236-251.
[34]	解艳玲，庄军. 鄂尔多斯盆地南部延安组砂体粒度特征[J]. 中国矿业大学学报，1998，27（4）：428-432. Xie Yanling, Zhuang Jun. Particle size and depositional environment of sandstone of Yan’an Formation in South Ordos Basin[J]. Journal of China University of Mining & Technology, 1998, 27(4): 428-432.
[35]	袁文芳，陈世悦，曾昌民，等. 柴达木盆地西部地区第三系碎屑岩粒度概率累积曲线特征[J]. 石油大学学报（自然科学版），2005，29（5）：12-18. Yuan Wenfang, Chen Shiyue, Zeng Changmin, et al. Probability cumulative grain size curves in terrigenous of the Tertiary in west Qaidam Basin[J]. Journal of the University of Petroleum, China, 2005, 29(5): 12-18.