假泥裂：上扬子地区下三叠统飞仙关组灰岩薄层中的网纹沉积构造

时志强; 彭深远; 王美玲; 乔丹; 时志强; 彭深远; 王美玲; 乔丹

doi:10.14027/j.issn.1000-0550.2023.032

[1]

曾允孚,夏文杰. 沉积岩石学[M]. 北京：地质出版社,1986.

Zeng Yunfu, Xia Wenjie. Sedimentary petrology[M]. Beijing: Geological Publishing House, 1986.

[2]

毛学刚,刘秀铭. 浅析中元古界和白垩系红层中泥裂的特征和古环境意义[J]. 亚热带资源与环境学报,2016,11（3）：20-28.

Mao Xuegang, Liu Xiuming. Preliminary analysis on characte-rization of mud-cracks in Meso-Proterozoic red beds and Cretaceous Danxia red beds and their paleo-environmental implications[J]. Journal of Subtropical Resources and Environment, 2016, 11(3): 20-28.

[3]

邓小杰,王冠,李越. 黔北桐梓志留系石牛栏组顶部特征指示的海岸线位置[J]. 地层学杂志,2012,36（4）：718-722.

Deng Xiaojie, Wang Guan, Li Yue. Sedimentary characteristics at the top of Shihniulan Formation (Late Aeronian, Silurian) and their implications for the identification of the paleo-shoreline in Tongzi, northern Guizhou[J]. Journal of Stratigraphy, 2012, 36(4): 718-722.

[4]

刘闯,钟建华,曹梦春,等. 甘肃敦煌地区现代泥裂几何学特征及成因机制探讨[J]. 高校地质学报,2018,24（1）：97-108.

Liu Chuang, Zhong Jianhua, Cao Mengchun, et al. Geometric features and genetic mechanism of modern mud cracks in Dunhuang, Gansu[J]. Geological Journal of China Universities, 2018, 24(1): 97-108.

[5]

许效松,万方,尹福光,等. 奥陶系宝塔组灰岩的环境相、生态相与成岩相[J]. 矿物岩石,2001,21（3）：64-68.

Xu Xiaosong, Wan Fang, Yin Fuguang, et al. Environment facies, ecological facies and diagenetic facies of Baota Formation, of Late Ordovician[J]. Journal of Mineralogy and Petrology, 2001, 21(3): 64-68.

[6]

刘育燕,杨巍然,森永速男,等. 华北陆块、秦岭地块和扬子陆块构造演化的古地磁证据[J]. 地质科技情报,1993,12（4）：17-21.

Liu Yuyan, Yang Weiran, Hayao Morinaga, et al. Paleogeographic history of North China continental block, Qinling geological block and Yangtze continental block since the Paleozoic Era[J]. Geological Science and Technology Information, 1993, 12(4): 17-21.

[7]

时志强,安红艳,伊海生,等. 上扬子地区早三叠世异常碳酸盐岩的分类与特征[J]. 古地理学报,2011,13（1）：1-10.

Shi Zhiqiang, An Hongyan, Yi Haisheng, et al. Classification and characters of the Early Triassic anomalous carbonate rocks in Upper Yangtze area[J]. Journal of Palaeogeography, 2011, 13(1): 1-10.

[8]

胡明毅,戴卿林,朱忠德,等. 中扬子地区海相碳酸盐岩石油地质特征及远景评价[J]. 石油与天然气地质,1993,14（4）：331-339.

Hu Mingyi, Dai Qinglin, Zhu Zhongde, et al. Petroleum geological characteristics and prospects assessment of marine carbonate rocks in Middle Yangzi River region[J]. Oil & Gas Geology, 1993, 14(4): 331-339.

[9]

马永生,傅强,郭彤楼,等. 川东北地区普光气田长兴—飞仙关气藏成藏模式与成藏过程[J]. 石油实验地质,2005,27（5）：35-41.

Ma Yongsheng, Fu Qiang, Guo Tonglou, et al. Pool forming pattern and process of the Upper Permian-Lower Triassic, the Puguang gas field, northeast Sichuan Basin, China[J]. Petroleum Geology & Experiment, 2005, 27(5): 35-41.

[10]

王一刚,张静,刘兴刚,等. 四川盆地东北部下三叠统飞仙关组碳酸盐蒸发台地沉积相[J]. 古地理学报,2005,7（3）：357-371.

Wang Yigang, Zhang Jing, Liu Xinggang, et al. Sedimentary facies of evaporative carbonate platform of the Feixianguan Formation of Lower Triassic in northeastern Sichuan Basin[J]. Journal of Palaeogeography, 2005, 7(3): 357-371.

[11]

王一刚,文应初,洪海涛,等. 四川盆地及邻区上二叠统—下三叠统海槽的深水沉积特征[J]. 石油与天然气地质,2006,27（5）：702-714.

Wang Yigang, Wen Yingchu, Hong Haitao, et al. Petroleum geological characteristics of deep water deposits in Upper Permian-Lower Triassic trough in Sichuan Basin and adjacent areas[J]. Oil & Gas Geology, 2006, 27(5): 702-714.

[12]

魏国齐,陈更生,杨威,等. 川北下三叠统飞仙关组“槽台”沉积体系及演化[J]. 沉积学报,2004,22（2）：254-260.

Wei Guoqi, Chen Gengsheng, Yang Wei, et al. Sedimentary system of platformal trough of Feixianguan Formation of Lower Triassic in northern Sichuan Basin and its evolution[J]. Acta Sedimentologica Sinica, 2004, 22(2): 254-260.

[13]

周慧,赵宗举,刘烨,等. 四川盆地及邻区早三叠世印度期层序岩相古地理及有利勘探区带[J]. 石油学报,2012,33（增刊2）：52-63.

Zhou Hui, Zhao Zongju, Liu Ye, et al. Sequence lithofacies paleogeography and favorable exploration zones of Induan Age of the Lower Triassic in Sichuan Basin and adjacent areas, China[J]. Acta Petrolei Sinica, 2012, 33(Suppl. 2): 52-63.

[14]

李子舜,詹立培,朱秀芳,等. 古生代—中生代之交的生物绝灭和地质事件：四川广元上寺二叠系—三叠系界线和事件的初步研究[J]. 地质学报,1986,60（1）：1-15.

Li Zishun, Zhan Lipei, Zhu Xiufang, et al. Mass extinction and geological events between Palaeozoic and Mesozoic Era[J]. Acta Geologica Sinica, 1986, 60(1): 1-15.

[15]

金若谷,黄恒铨. 四川广元上寺二叠系—三叠系界线剖面沉积特征及环境演变[C]//中国地质学会. 地层古生物论文集(第十八辑). 北京：地质出版社,1987：37-80.

Jin Ruogu, Huang Hengquan. Sedimentary features and environmental evolution of the Permian-Triassic boundary section in Shangsi, Guangyuan, Sichuan province[C]//Geological Society of China. Professional papers of stratigraphy and palaeontology (No. 18). Beijing: Geological Publishing House, 1987: 37-80.

[16]

孙春燕,胡明毅,胡忠贵,等. 四川盆地下三叠统飞仙关组层序—岩相古地理特征[J]. 海相油气地质,2015,20（3）：1-9.

Sun Chunyan, Hu Mingyi, Hu Zhonggui, et al. Sequence-based lithofacies and paleogeography of Lower Triassic Feixianguan Formation in Sichuan Basin[J]. Marine Origin Petroleum Geology, 2015, 20(3): 1-9.

[17]

崔卫东. 川西北地区下三叠统飞仙关组沉积、成岩作用及其对储层的影响[D]. 成都：西南石油学院,2003.

Cui Weidong. The sedimentation, diagenesis and its influence upon the reservoir of Feixianguan Formation in Lower Triassic series, northwest Sichuan[D]. Chengdu: Southwest Petroleum University, 2003.

[18]

四川省地质局第2区测队. 广元幅I-48-34 1/20万区域地质测量报告[R]. 成都：四川省地质局第2区测队,1966.

Area 2 Survey Team of Sichuan Provincial Geological Bureau. Regional geological survey memoir, 1: 20000 Guanguan image[R]. Chengdu: Area 2 Survey Team of Sichuan Provincial Geological Bureau, 1996.

[19]

金若谷,沈桂梅,须湘官,等. 四川广元二叠系—三叠系界线黏土岩沉积特征及成因探讨[J]. 岩石矿物学杂志,1986,5（2）：107-118.

Jin Ruogu, Shen Guimei, Xu Xiangguan, et al. Sedimentary characters and origin of the boundary clay rocks of Permo-Triassic in the region of Guangyuan, Sichuan province[J]. Acta Petrologica et Mineralogica, 1986, 5(2): 107-118.

[20]

黄思静. 上扬子二叠系─三叠系初海相碳酸盐岩的碳同位素组成与生物绝灭事件[J]. 地球化学,1994,23（1）：60-68.

Huang Sijing. Carbon isotopes of Permian and Permian-Triassic boundary in Upper Yangtze Platform and the mass extinction[J]. Geochimica, 1994, 23(1): 60-68.

[21]

曾德勇,时志强,张华,等. 广元上寺剖面下三叠统飞仙关组风暴岩：巨型季风体制下的极端气候事件?[J]. 沉积学报,2011,29（3）：440-448.

Zeng Deyong, Shi Zhiqiang, Zhang Hua, et al. Tempestite of Early Triassic Feixianguan Formation in Shangsi section, Guangyuan: Are they extreme climatic event under megamonsoon system?[J]. Acta Sedimentologica Sinica, 2011, 29(3): 440-448.

[22]

赵永胜,王多义,胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境[J]. 沉积学报,1994,12（2）：1-9.

Zhao Yongsheng, Wang Duoyi, Hu Zhishui. Sedimentology and environment of carbonate gravity flows on the western margin of Lower Triassic, Sichuan Basin[J]. Acta Sedimentologica Sinica, 1994, 12(2): 1-9.

[23]

Wignall P B, Twitchett R J. Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction[J]. Sedimentology, 1999, 46(2): 303-316.

[24]

Hallam A. Why was there a delayed radiation after the end-Palaeozoic extinctions?[J]. Historical Biology, 1991, 5(2/3/4): 257-262.

[25]

Parrish J T, Peterson F. Wind directions predicted from global circulation models and wind directions determined from eolian sandstones of the western United States: A comparison[J]. Sedimentary Geology, 1988, 56(1/2/3/4): 261-282.

[26]

时志强,曾德勇,熊兆军,等. 三叠纪巨型季风在上扬子地区的沉积学记录[J]. 矿物岩石地球化学通报,2010,29（2）：164-172.

Shi Zhiqiang, Zeng Deyong, Xiong Zhaojun, et al. Sedimentary records of Triassic megamonsoon in Upper Yangtze area[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2010, 29(2): 164-172.

[27]

Berner R A. GEOCARBSULF: A combined model for Phanerozoic atmospheric O₂ and CO₂[J]. Geochimica et Cosmochimica Acta, 2006, 70(23): 5653-5664.

[28]

Sun Y D, Joachimski M M, Wignall P B, et al. Lethally hot temperatures during the Early Triassic greenhouse[J]. Science, 2012, 338(6105): 366-370.

[29]

赵小明,牛志军,童金南,等. 早三叠世生物复苏期的特殊沉积：“错时相”沉积[J]. 沉积学报,2010,28（2）：314-323.

Zhao Xiaoming, Niu Zhijun, Tong Jinnan, et al. The distinctive sediments in the Early Triassic recovery time: “anachronistic facies”[J]. Acta Sedimentologica Sinica, 2010, 28(2): 314-323.

[30]

Duke W L. Hummocky cross-stratification, tropical hurricanes, and intense winter storms[J]. Sedimentology, 1985, 32(2): 167-194.

[31]

Barron E J. Severe storms during Earth history[J]. GSA Bulletin, 1989, 101(5): 601-612.

[32]

Kidder D L, Worsley T R. Causes and consequences of extreme Permo-Triassic warming to globally equable climate and relation to the Permo-Triassic extinction and recovery[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 203(3/4): 207-237.

[33]

许安涛,李凤杰,刘奎,等. 北川甘溪下泥盆统风暴岩沉积特征及其沉积模式[J]. 中国地质,2018,45（5）：1049-1061.

Xu Antao, Li Fengjie, Liu Kui, et al. The characteristics and sedimentary model of storm deposits in the Lower Devonian strata of Beichuan[J]. Geology in China, 2018, 45(5): 1049-1061.

[34]

吝文,姜在兴,向树安,等. 鄂尔多斯盆地大牛地气田下二叠统下石盒子组盒2及盒3段风暴岩研究[J]. 古地理学报,2008,10（2）：167-174.

Lin Wen, Jiang Zaixing, Xiang Shu’an, et al. Researches on tempestites of the member 2 and member 3 of Lower Permian Xiashihezi Formation in Daniudi gasfield, Ordos Basin[J]. Journal of Palaeogeography, 2008, 10(2): 167-174.

[35]

廖纪佳,马思豪,廖明光,等. 奥陶系宝塔灰岩网纹构造成因研究进展及新发现[J]. 沉积学报,2017,35（2）：241-252.

Liao Jijia, Ma Sihao, Liao Mingguang, et al. Research of the origin of network structure in the Ordovician Pagoda limestone: Advances and new discovery[J]. Acta Sedimentologica Sinica, 2017, 35(2): 241-252.

[36]

沈建伟. 贵州及邻区宝塔组灰岩成因的新观察[J]. 贵州地质,1989,6（1）：35-38,22.

Shen Jianwei. New observations of the origin of Baota limestone in Guizhou and its adjacent regions[J]. Guizhou Geology, 1989, 6(1): 35-38, 22.

[37]

周书欣,王建国. 贵州石阡地区宝塔灰岩的成因[J]. 石油实验地质,1992,14（3）：291-295,326.

Zhou Shuxin, Wang Jianguo. On the origin of Pagoda stones in the Shiqian region, Guizhou province[J]. Experimental Petroleum Geology, 1992, 14(3): 291-295, 326.

[38]

Cowan C A, James N P. Diastasis cracks: Mechanically generated synaeresis-like cracks in Upper Cambrian shallow water oolite and ribbon carbonates[J]. Sedimentology, 1992, 39(6): 1101-1118.

[39]

戎嘉余,陈旭. 华南晚奥陶世的动物群分异及生物相、岩相分布模式[J]. 古生物学报,1987,26（5）：507-535.

Rong Jiayu, Chen Xu. Faunal differentiation, biofacies and lithofacies pattern of Late Ordovician (Ashgillian) in South China[J]. Acta Palaeontologica Sinica, 1987, 26(5): 507-535.

[40]

王尧. 上扬子地台中奥陶统“龟裂纹”灰岩成因的新解释[J]. 地质科学,1995,30（3）：268-274.

Wang Yao. Middle Ordovician cracked limestones of polygonal structure in the Upper Yangtze River area, South China: A new interpretation of their origin[J]. Chinese Journal of Geology, 1995, 30(3): 268-274.

[1]	曾允孚,夏文杰. 沉积岩石学[M]. 北京：地质出版社,1986. Zeng Yunfu, Xia Wenjie. Sedimentary petrology[M]. Beijing: Geological Publishing House, 1986.
[2]	毛学刚,刘秀铭. 浅析中元古界和白垩系红层中泥裂的特征和古环境意义[J]. 亚热带资源与环境学报,2016,11（3）：20-28. Mao Xuegang, Liu Xiuming. Preliminary analysis on characte-rization of mud-cracks in Meso-Proterozoic red beds and Cretaceous Danxia red beds and their paleo-environmental implications[J]. Journal of Subtropical Resources and Environment, 2016, 11(3): 20-28.
[3]	邓小杰,王冠,李越. 黔北桐梓志留系石牛栏组顶部特征指示的海岸线位置[J]. 地层学杂志,2012,36（4）：718-722. Deng Xiaojie, Wang Guan, Li Yue. Sedimentary characteristics at the top of Shihniulan Formation (Late Aeronian, Silurian) and their implications for the identification of the paleo-shoreline in Tongzi, northern Guizhou[J]. Journal of Stratigraphy, 2012, 36(4): 718-722.
[4]	刘闯,钟建华,曹梦春,等. 甘肃敦煌地区现代泥裂几何学特征及成因机制探讨[J]. 高校地质学报,2018,24（1）：97-108. Liu Chuang, Zhong Jianhua, Cao Mengchun, et al. Geometric features and genetic mechanism of modern mud cracks in Dunhuang, Gansu[J]. Geological Journal of China Universities, 2018, 24(1): 97-108.
[5]	许效松,万方,尹福光,等. 奥陶系宝塔组灰岩的环境相、生态相与成岩相[J]. 矿物岩石,2001,21（3）：64-68. Xu Xiaosong, Wan Fang, Yin Fuguang, et al. Environment facies, ecological facies and diagenetic facies of Baota Formation, of Late Ordovician[J]. Journal of Mineralogy and Petrology, 2001, 21(3): 64-68.
[6]	刘育燕,杨巍然,森永速男,等. 华北陆块、秦岭地块和扬子陆块构造演化的古地磁证据[J]. 地质科技情报,1993,12（4）：17-21. Liu Yuyan, Yang Weiran, Hayao Morinaga, et al. Paleogeographic history of North China continental block, Qinling geological block and Yangtze continental block since the Paleozoic Era[J]. Geological Science and Technology Information, 1993, 12(4): 17-21.
[7]	时志强,安红艳,伊海生,等. 上扬子地区早三叠世异常碳酸盐岩的分类与特征[J]. 古地理学报,2011,13（1）：1-10. Shi Zhiqiang, An Hongyan, Yi Haisheng, et al. Classification and characters of the Early Triassic anomalous carbonate rocks in Upper Yangtze area[J]. Journal of Palaeogeography, 2011, 13(1): 1-10.
[8]	胡明毅,戴卿林,朱忠德,等. 中扬子地区海相碳酸盐岩石油地质特征及远景评价[J]. 石油与天然气地质,1993,14（4）：331-339. Hu Mingyi, Dai Qinglin, Zhu Zhongde, et al. Petroleum geological characteristics and prospects assessment of marine carbonate rocks in Middle Yangzi River region[J]. Oil & Gas Geology, 1993, 14(4): 331-339.
[9]	马永生,傅强,郭彤楼,等. 川东北地区普光气田长兴—飞仙关气藏成藏模式与成藏过程[J]. 石油实验地质,2005,27（5）：35-41. Ma Yongsheng, Fu Qiang, Guo Tonglou, et al. Pool forming pattern and process of the Upper Permian-Lower Triassic, the Puguang gas field, northeast Sichuan Basin, China[J]. Petroleum Geology & Experiment, 2005, 27(5): 35-41.
[10]	王一刚,张静,刘兴刚,等. 四川盆地东北部下三叠统飞仙关组碳酸盐蒸发台地沉积相[J]. 古地理学报,2005,7（3）：357-371. Wang Yigang, Zhang Jing, Liu Xinggang, et al. Sedimentary facies of evaporative carbonate platform of the Feixianguan Formation of Lower Triassic in northeastern Sichuan Basin[J]. Journal of Palaeogeography, 2005, 7(3): 357-371.
[11]	王一刚,文应初,洪海涛,等. 四川盆地及邻区上二叠统—下三叠统海槽的深水沉积特征[J]. 石油与天然气地质,2006,27（5）：702-714. Wang Yigang, Wen Yingchu, Hong Haitao, et al. Petroleum geological characteristics of deep water deposits in Upper Permian-Lower Triassic trough in Sichuan Basin and adjacent areas[J]. Oil & Gas Geology, 2006, 27(5): 702-714.
[12]	魏国齐,陈更生,杨威,等. 川北下三叠统飞仙关组“槽台”沉积体系及演化[J]. 沉积学报,2004,22（2）：254-260. Wei Guoqi, Chen Gengsheng, Yang Wei, et al. Sedimentary system of platformal trough of Feixianguan Formation of Lower Triassic in northern Sichuan Basin and its evolution[J]. Acta Sedimentologica Sinica, 2004, 22(2): 254-260.
[13]	周慧,赵宗举,刘烨,等. 四川盆地及邻区早三叠世印度期层序岩相古地理及有利勘探区带[J]. 石油学报,2012,33（增刊2）：52-63. Zhou Hui, Zhao Zongju, Liu Ye, et al. Sequence lithofacies paleogeography and favorable exploration zones of Induan Age of the Lower Triassic in Sichuan Basin and adjacent areas, China[J]. Acta Petrolei Sinica, 2012, 33(Suppl. 2): 52-63.
[14]	李子舜,詹立培,朱秀芳,等. 古生代—中生代之交的生物绝灭和地质事件：四川广元上寺二叠系—三叠系界线和事件的初步研究[J]. 地质学报,1986,60（1）：1-15. Li Zishun, Zhan Lipei, Zhu Xiufang, et al. Mass extinction and geological events between Palaeozoic and Mesozoic Era[J]. Acta Geologica Sinica, 1986, 60(1): 1-15.
[15]	金若谷,黄恒铨. 四川广元上寺二叠系—三叠系界线剖面沉积特征及环境演变[C]//中国地质学会. 地层古生物论文集(第十八辑). 北京：地质出版社,1987：37-80. Jin Ruogu, Huang Hengquan. Sedimentary features and environmental evolution of the Permian-Triassic boundary section in Shangsi, Guangyuan, Sichuan province[C]//Geological Society of China. Professional papers of stratigraphy and palaeontology (No. 18). Beijing: Geological Publishing House, 1987: 37-80.
[16]	孙春燕,胡明毅,胡忠贵,等. 四川盆地下三叠统飞仙关组层序—岩相古地理特征[J]. 海相油气地质,2015,20（3）：1-9. Sun Chunyan, Hu Mingyi, Hu Zhonggui, et al. Sequence-based lithofacies and paleogeography of Lower Triassic Feixianguan Formation in Sichuan Basin[J]. Marine Origin Petroleum Geology, 2015, 20(3): 1-9.
[17]	崔卫东. 川西北地区下三叠统飞仙关组沉积、成岩作用及其对储层的影响[D]. 成都：西南石油学院,2003. Cui Weidong. The sedimentation, diagenesis and its influence upon the reservoir of Feixianguan Formation in Lower Triassic series, northwest Sichuan[D]. Chengdu: Southwest Petroleum University, 2003.
[18]	四川省地质局第2区测队. 广元幅I-48-34 1/20万区域地质测量报告[R]. 成都：四川省地质局第2区测队,1966. Area 2 Survey Team of Sichuan Provincial Geological Bureau. Regional geological survey memoir, 1: 20000 Guanguan image[R]. Chengdu: Area 2 Survey Team of Sichuan Provincial Geological Bureau, 1996.
[19]	金若谷,沈桂梅,须湘官,等. 四川广元二叠系—三叠系界线黏土岩沉积特征及成因探讨[J]. 岩石矿物学杂志,1986,5（2）：107-118. Jin Ruogu, Shen Guimei, Xu Xiangguan, et al. Sedimentary characters and origin of the boundary clay rocks of Permo-Triassic in the region of Guangyuan, Sichuan province[J]. Acta Petrologica et Mineralogica, 1986, 5(2): 107-118.
[20]	黄思静. 上扬子二叠系─三叠系初海相碳酸盐岩的碳同位素组成与生物绝灭事件[J]. 地球化学,1994,23（1）：60-68. Huang Sijing. Carbon isotopes of Permian and Permian-Triassic boundary in Upper Yangtze Platform and the mass extinction[J]. Geochimica, 1994, 23(1): 60-68.
[21]	曾德勇,时志强,张华,等. 广元上寺剖面下三叠统飞仙关组风暴岩：巨型季风体制下的极端气候事件?[J]. 沉积学报,2011,29（3）：440-448. Zeng Deyong, Shi Zhiqiang, Zhang Hua, et al. Tempestite of Early Triassic Feixianguan Formation in Shangsi section, Guangyuan: Are they extreme climatic event under megamonsoon system?[J]. Acta Sedimentologica Sinica, 2011, 29(3): 440-448.
[22]	赵永胜,王多义,胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境[J]. 沉积学报,1994,12（2）：1-9. Zhao Yongsheng, Wang Duoyi, Hu Zhishui. Sedimentology and environment of carbonate gravity flows on the western margin of Lower Triassic, Sichuan Basin[J]. Acta Sedimentologica Sinica, 1994, 12(2): 1-9.
[23]	Wignall P B, Twitchett R J. Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction[J]. Sedimentology, 1999, 46(2): 303-316.
[24]	Hallam A. Why was there a delayed radiation after the end-Palaeozoic extinctions?[J]. Historical Biology, 1991, 5(2/3/4): 257-262.
[25]	Parrish J T, Peterson F. Wind directions predicted from global circulation models and wind directions determined from eolian sandstones of the western United States: A comparison[J]. Sedimentary Geology, 1988, 56(1/2/3/4): 261-282.
[26]	时志强,曾德勇,熊兆军,等. 三叠纪巨型季风在上扬子地区的沉积学记录[J]. 矿物岩石地球化学通报,2010,29（2）：164-172. Shi Zhiqiang, Zeng Deyong, Xiong Zhaojun, et al. Sedimentary records of Triassic megamonsoon in Upper Yangtze area[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2010, 29(2): 164-172.
[27]	Berner R A. GEOCARBSULF: A combined model for Phanerozoic atmospheric O₂ and CO₂[J]. Geochimica et Cosmochimica Acta, 2006, 70(23): 5653-5664.
[28]	Sun Y D, Joachimski M M, Wignall P B, et al. Lethally hot temperatures during the Early Triassic greenhouse[J]. Science, 2012, 338(6105): 366-370.
[29]	赵小明,牛志军,童金南,等. 早三叠世生物复苏期的特殊沉积：“错时相”沉积[J]. 沉积学报,2010,28（2）：314-323. Zhao Xiaoming, Niu Zhijun, Tong Jinnan, et al. The distinctive sediments in the Early Triassic recovery time: “anachronistic facies”[J]. Acta Sedimentologica Sinica, 2010, 28(2): 314-323.
[30]	Duke W L. Hummocky cross-stratification, tropical hurricanes, and intense winter storms[J]. Sedimentology, 1985, 32(2): 167-194.
[31]	Barron E J. Severe storms during Earth history[J]. GSA Bulletin, 1989, 101(5): 601-612.
[32]	Kidder D L, Worsley T R. Causes and consequences of extreme Permo-Triassic warming to globally equable climate and relation to the Permo-Triassic extinction and recovery[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 203(3/4): 207-237.
[33]	许安涛,李凤杰,刘奎,等. 北川甘溪下泥盆统风暴岩沉积特征及其沉积模式[J]. 中国地质,2018,45（5）：1049-1061. Xu Antao, Li Fengjie, Liu Kui, et al. The characteristics and sedimentary model of storm deposits in the Lower Devonian strata of Beichuan[J]. Geology in China, 2018, 45(5): 1049-1061.
[34]	吝文,姜在兴,向树安,等. 鄂尔多斯盆地大牛地气田下二叠统下石盒子组盒2及盒3段风暴岩研究[J]. 古地理学报,2008,10（2）：167-174. Lin Wen, Jiang Zaixing, Xiang Shu’an, et al. Researches on tempestites of the member 2 and member 3 of Lower Permian Xiashihezi Formation in Daniudi gasfield, Ordos Basin[J]. Journal of Palaeogeography, 2008, 10(2): 167-174.
[35]	廖纪佳,马思豪,廖明光,等. 奥陶系宝塔灰岩网纹构造成因研究进展及新发现[J]. 沉积学报,2017,35（2）：241-252. Liao Jijia, Ma Sihao, Liao Mingguang, et al. Research of the origin of network structure in the Ordovician Pagoda limestone: Advances and new discovery[J]. Acta Sedimentologica Sinica, 2017, 35(2): 241-252.
[36]	沈建伟. 贵州及邻区宝塔组灰岩成因的新观察[J]. 贵州地质,1989,6（1）：35-38,22. Shen Jianwei. New observations of the origin of Baota limestone in Guizhou and its adjacent regions[J]. Guizhou Geology, 1989, 6(1): 35-38, 22.
[37]	周书欣,王建国. 贵州石阡地区宝塔灰岩的成因[J]. 石油实验地质,1992,14（3）：291-295,326. Zhou Shuxin, Wang Jianguo. On the origin of Pagoda stones in the Shiqian region, Guizhou province[J]. Experimental Petroleum Geology, 1992, 14(3): 291-295, 326.
[38]	Cowan C A, James N P. Diastasis cracks: Mechanically generated synaeresis-like cracks in Upper Cambrian shallow water oolite and ribbon carbonates[J]. Sedimentology, 1992, 39(6): 1101-1118.
[39]	戎嘉余,陈旭. 华南晚奥陶世的动物群分异及生物相、岩相分布模式[J]. 古生物学报,1987,26（5）：507-535. Rong Jiayu, Chen Xu. Faunal differentiation, biofacies and lithofacies pattern of Late Ordovician (Ashgillian) in South China[J]. Acta Palaeontologica Sinica, 1987, 26(5): 507-535.
[40]	王尧. 上扬子地台中奥陶统“龟裂纹”灰岩成因的新解释[J]. 地质科学,1995,30（3）：268-274. Wang Yao. Middle Ordovician cracked limestones of polygonal structure in the Upper Yangtze River area, South China: A new interpretation of their origin[J]. Chinese Journal of Geology, 1995, 30(3): 268-274.