|Table of Contents|

Carbon and Oxygen Isotopic Characteristics of Lacustrine Carbonate Rocks from the First Member of Paleogene Bianqiao Formation in Pingyi Basin of Shandong, China and Their Geological Significance(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2020年第03期
Page:
342-354
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Carbon and Oxygen Isotopic Characteristics of Lacustrine Carbonate Rocks from the First Member of Paleogene Bianqiao Formation in Pingyi Basin of Shandong, China and Their Geological Significance
Author(s):
JIA Yu1; 2;  HUANG Wen-hui1; 2*
(1. Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism of Ministry of Education, China University of Geosciences, Beijing 100083, China; 2. School of Energy Resources, China University of Geosciences, Beijing 100083, China)
Keywords:
geochemistry;  lacustrine carbonate rock;  carbon and oxygen isotopes;  paleosalinity;  paleoclimate;  Paleogene;  Bianqiao Formation;  Shandong
PACS:
P588.24+5; P597+.2
DOI:
10.19814/j.jese.2019.12030
Abstract:
The lithological characteristics, carbon and oxygen isotopic composition, major and trace elements of 19 samples for lacustrine carbonate rocks from the first member of Paleogene Bianqiao Formation in Pingyi Basin of Shandong were analyzed. The results show that the lithological changes from the bottom to the top of the first member of Paleogene Bianqiao Formation in Pingyi Basin are coarse clastic rock, oncolite limestone, bioclastic limestone, grain limestone, micrite limestone/marlstone. The δ13C values of carbonate rocks are -3.5‰--2.5‰ with an average of -2.9‰, δ18O values are -8.5‰--6.5‰ with an average of -7.6‰, and the carbon and oxygen isotopes show good positive correlation, suggesting a relative closed lake system with a relatively long resident time at Paleogene in Pingyi Basin. The Sr/Ba ratios of carbonate rocks are 0.25-31.55, and it can be considered that the aqueous medium at Paleogene in Pingyi Basin is mainly salt water; the Mg/Ca ratios are 0.004 2-0.011 9, revealing that the paleoclimate evolution at Paleogene in Pingyi Basin experiences 3 stages, including humid climate→semiarid climate→arid climate. According to the vertical evolution of lithologic variation and thin section characteristics, it can be inferred that the hydrodynamic force of lake basin gradually weakens as strata becoming upper, and the water body of lake basin gradually converts from high-energy to low-energy environment at Paleogene in Pingyi Basin.

References:

[1] 沈安江,陈娅娜,蒙绍兴,等.中国海相碳酸盐岩储层研究进展及油气勘探意义[J].海相油气地质,2019,24(4):1-14.
SHEN An-jiang,CHEN Ya-na,MENG Shao-xing,et al.The Research Progress of Marine Carbonate Reservoirs in China and Its Significance for Oil and Gas Exploration[J].Marine Origin Petroleum Geology,2019,24(4):1-14.
[2] 马永生,何治亮,赵培荣,等.深层—超深层碳酸盐岩储层形成机理新进展[J].石油学报,2019,40(12):1415-1425.
MA Yong-sheng,HE Zhi-liang,ZHAO Pei-rong,et al.A New Progress in Formation Mechanism of Deep and Ultra-deep Carbonate Reservoirs[J].Acta Petrolei Sinica,2019,40(12):1415-1425.
[3] 李 阳,康志江,薛兆杰,等.中国碳酸盐岩油气藏开发理论与实践[J].石油勘探与开发,2018,45(4):669-678.
LI Yang,KANG Zhi-jiang,XUE Zhao-jie,et al.Theories and Practices of Carbonate Reservoirs Development in China[J].Petroleum Exploration and Deve-lopment,2018,45(4):669-678.
[4] 陈欢庆,胡海燕,李文青,等.复杂岩性油藏精细描述研究进展[J].地球科学与环境学报,2020,42(1):99-119.
CHEN Huan-qing,HU Hai-yan,LI Wen-qing,et al.Review on Fine Description of Complex Lithologic Reservoir[J].Journal of Earth Sciences and Environment,2020,42(1):99-119.
[5] 刘树根,宋金民,罗 平,等.四川盆地深层微生物碳酸盐岩储层特征及其油气勘探前景[J].成都理工大学学报(自然科学版),2016,43(2):129-152.
LIU Shu-gen,SONG Jin-min,LUO Ping,et al.Cha-racteristics of Microbial Carbonate Reservoir and Its Hydrocarbon Exploring Outlook in the Sichuan Basin,China[J].Journal of Chengdu University of Technology(Science and Technology Edition),2016,43(2):129-152.
图7 湖相碳酸盐岩显微照片
Fig.7 Microphotographs of Lacustrine Carbonate Rocks[6] 杜江民,龙鹏宇,杨 鹏,等.中国陆相湖盆碳酸盐岩储集层特征及其成藏条件[J].地球科学进展,2020,35(1):52-69.
DU Jiang-min,LONG Peng-yu,YANG Peng,et al.Cha-racteristics of Carbonate Reservoir and Its Forming Conditions in Continental Lake Basin of China[J].Advances in Earth Science,2020,35(1):52-69.
[7] 苏 玲,朱如凯,崔景伟,等.中国湖相碳酸盐岩时空分布与碳同位素特征[J].古地理学报,2017,19(6):1064-1076.
SU Ling,ZHU Ru-kai,CUI Jing-wei,et al.Spatial-temporal Distribution of Lacustrine Carbonate Rocks in China and Their Carbon and Oxygen Isotopic Cha-racteristics[J].Journal of Palaeogeography,2017,19(6):1064-1076.
[8] 韩剑发,苏 洲,陈利新,等.塔里木盆地台盆区走滑断裂控储控藏作用及勘探潜力[J].石油学报,2019,40(11):1296-1310.
HAN Jian-fa,SU Zhou,CHEN Li-xin,et al.Reservoir-controlling and Accumulation-controlling of Strike-slip Faults and Exploration Potential in the Platform of Tarim Basin[J].Acta Petrolei Sinica,2019,40(11):1296-1310.
[9] 贾文博,关 平,刘沛显,等.湖相碳酸盐岩元素测试方法研究[J].沉积学报,2018,36(4):842-852.
JIA Wen-bo,GUAN Ping,LIU Pei-xian,et al.Study on the Element Testing Method of Lacustrine Carbonates[J].Acta Sedimentologica Sinica,2018,36(4):842-852.
[10] 赵永胜,赵霞飞.内陆湖泊贝壳碳酸盐碳氧同位素组成与古气候研究[J].成都地质学院学报,1990,17(3):83-93.
ZHAO Yong-sheng,ZHAO Xia-fei.The Approach of Paleoclimate and the Oxygen,Carbon Isotopic Compositions of Shelly Carbonates in Inland Lake[J].Journal of Chengdu College of Geology,1990,17(3):83-93.
[11] 王腾飞,金振奎,GUNAY A,等.湖盆滩坝沉积研究进展[J].科技导报,2018,36(23):57-67.
WANG Teng-fei,JIN Zhen-kui,GUNAY A,et al.Research Progress of Lacustrine Beach-bars[J].Science and Technology Review,2018,36(23):57-67.
[12] RYDER R T,FOUCH T D,ELISON J H.Early Tertiary Sedimentation in the Western Uinta Basin,Utah[J].GSA Bulletin,1976,87(4):496-512.
[13] STUIVER M.Oxygen and Carbon Isotope Ratios of Fresh-water Carbonates as Climate Indicators[J].Journal of Geophysical Resarch,1970,75(27):5247-5257.
[14] 王衡鉴,周书欣,滕玉洪,等.松辽盆地西部中部组合淡水碳酸盐岩的分布规律及其与油气的关系[J].大庆石油学院学报,1983(1):35-49.
WANG Heng-jian,ZHOU Shu-xin,TENG Yu-hong,et al.Distribution of Freshwater Carbonates in the Middle Part of the Western Part of Songliao Basin and Its Relationship with Oil and Gas[J].Journal of Daqing Petroleum Institute,1983(1):35-49
[15] 周自立,杜韫华.湖相碳酸盐岩的沉积相与油气分布关系:以山东胜利油田下第三系碳酸盐岩为例[J].石油实验地质,1986,8(2):123-132.
ZHOU Zi-li,DU Yun-hua.Relationship Between Sedimentary Facies of Lacustrine Carbonate Rocks and Oil and Gas Distribution[J].Experimental Petroleum Geo-logy,1986,8(2):123-132.
[16] 潘文静,王清斌,刘士磊,等.渤海海域石臼坨地区古近系沙河街组湖相生屑白云岩成因[J].古地理学报,2017,19(5):835-848.
PAN Wen-jing,WANG Qing-bin,LIU Shi-lei,et al.Origin of Lacustrine Bioclastic Dolostone in the Paleogene Shahejie Formation:A Case Study in Shijiutuo Area,Bohai Sea[J].Journal of Palaeogeography,2017,19(5):835-848.
[17] 毛玲玲,伊海生,季长军,等.柴达木盆地新生代湖相碳酸盐岩岩石学及碳氧同位素特征[J].地质科技情报,2014,33(1):41-48.
MAO Ling-ling,YI Hai-sheng,JI Chang-jun,et al.Petrography and Carbon-oxygen Isotope Characteristics of the Cenozoic Lacustrine Carbonate Rocks in Qaidam Basin[J].Geological Science and Technology Information,2014,33(1):41-48.
[18] 袁剑英,黄成刚,曹正林,等.咸化湖盆白云岩碳氧同位素特征及古环境意义:以柴西地区始新统下干柴沟组为例[J].地球化学,2015,44(3):254-266.
YUAN Jian-ying,HUANG Cheng-gang,CAO Zheng-lin,et al.Carbon and Oxygen Isotopic Composition of Saline Lacustrine Dolomite and Its Palaeoenvironmental Significance:A Case Study of Lower Eocene Ganchaigou Formation in Western Qaidam Basin[J].Geochimica,2015,44(3):254-266.
[19] YI S,HUANG W H,MU N N.Lacustrine Carbonates of Paleogene in Zhanhua Sag,Bohai Bay Basin,East China[J].Carbonates and Evaporites,2019,34(3):1157-1173.
[20] LI S Y,CURRIE B S,ROWLEY D B,et al.Diagenesis of Shallowly Buried Miocene Lacustrine Carbonates from the Hoh Xil Basin,Northern Tibetan Plateau:Implications for Stable-isotope Based Elevation Estimates[J].Sedimentary Geology,2019,388:20-36.
[21] 曹高社,余爽杰,孙凤余,等.豫西宜阳地区三叠纪早期孙家沟组上段湖相碳酸盐岩碳氧同位素和古环境分析[J].地质学报,2019,93(5):1137-1153.
CAO Gao-she,YU Shuang-jie,SUN Feng-yu,et al.Carbon and Oxygen Isotopic Composition and Palaeoenvironment Analysis of Lacustrine Carbonate Rocks in the Upper Member of Early Triassic Sunjiagou Formation,Yiyang Area,Western Henan Province[J].Acta Geologica Sinica,2019,93(5):1137-1153.
[22] MCCORMACK J,NEHRKE G,JONS N,et al.Refining the Interpretation of Lacustrine Carbonate Isotope Records:Implications of a Mineralogy-specific Lake Van Case Study[J].Chemical Geology,2019,513:167-183.
[23] 何起祥.碳、氧稳定同位素在沉积学中的应用[J].世界地质,1983,2(1):1-14.
HE Qi-xiang.Application of Carbon-oxygen Isotope in Sedimentology[J].Global Geology,1983,2(1):1-14.
[24] 张秀莲.碳酸盐岩中氧、碳稳定同位素与古盐度、古水温的关系[J].沉积学报,1985,3(4):17-30.
ZHANG Xiu-lian.Relationship Between Carbon and Oxygen Stable Isotope in Carbonate Rocks and Paleo-salinity and Paleotemperature of Seawater[J].Acta Sedimentologica Sinica,1985,3(4):17-30.
[25] 邵龙义.碳酸盐岩氧、碳同位素与古温度等的关系[J].中国矿业大学学报,1994,23(1):39-45.
SHAO Long-yi.The Relation of the Oxygen and Carbon Isotope in the Carbonate Rocks to the Paleotemperature[J].Journal of China University of Mining and Technology,1994,23(1):39-45.
[26] 刘传联.东营凹陷沙河街组湖相碳酸盐岩碳氧同位素组分及其古湖泊学意义[J].沉积学报,1998,16(3):109-114.
LIU Chuan-lian.Carbon and Oxygen Isotopic Compositions of Lacustrine Carbonates of the Shahejie Formation in the Dongying Depression and Their Paleo-limnological Significance[J].Acta Sedimentologica Sinica,1998,16(3):109-114.
[27] 万友利,王 剑,付修根,等.羌塘盆地南坳陷中侏罗统布曲组白云岩储层成因流体同位素地球化学示踪[J].石油与天然气地质,2020,41(1):189-200.
WAN You-li,WANG Jian,FU Xiu-gen,et al.Geochemical Tracing of Isotopic Fluid of Dolomite Reservoir in the Middle Jurassic Buqu Formation in Southern Depression of Qiangtang Basin[J].Oil and Gas Geology,2020,41(1):189-200.
[28] 杨永恒,孙国强,王晔桐,等.柴达木盆地北缘平台地区路乐河组沉积环境与成岩流体特征[J].沉积学报,2019,37(6):1258-1268.
YANG Yong-heng,SUN Guo-qiang,WANG Ye-tong,et al.Sedimentary Diagenetic Environment of the Lulehe Formation in the Pingtai Region,Northern Qaidam Basin[J].Acta Sedimentologica Sinica,2019,37(6):1258-1268.
[29] 李熙哲,管守锐,谢庆宾,等.平邑盆地下第三系官中段核形石成因分析[J].岩石学报,2000,16(2):262-268.
LI Xi-zhe,GUAN Shou-rui,XIE Qing-bin,et al.The Oncoids Genesis in the Middle Member of the Guan-zhuang Formation of Eocene in Pingyi Basin[J].Acta Petrologica Sinica,2000,16(2):262-268.
[30] 顾澄皋.山东平邑盆地下第三系钙壳的特征及意义[J].沉积学报,1988,6(3):89-97.
GU Cheng-gao.Characteristics and Significance of Lower Tertiary Caliches in the Pingyi Basin,Shandong Pro-vince[J].Acta Sedimentologica Sinica,1988,6(3):89-97.
[31] 潘文静,杜晓峰,王清斌,等.渤海海域东南部新近纪湖盆萎缩期古生物特征及古环境意义[J].微体古生物学报,2018,35(3):238-250.
PAN Wen-jing,DU Xiao-feng,WANG Qing-bin,et al.Neocene Palaeontological Characteristics and Its Paleoenvironment Significance During the Withering Period of the Lacustrine Basin in the Southeastern Bohai Sea,North China[J].Acta Micropalaeontolagica Sinica,2018,35(3):238-250.
[32] 董俊昌,李 燕,孙维凤,等.平邑盆地官庄群湖相碳酸盐岩的古地理意义[J].地质与勘探,2012,48(1):93-101.
DONG Jun-chang,LI Yan,SUN Wei-feng,et al.Paleo-geographic Significance of Guanzhuang Group Lacustrine Carbonate in the Pingyi Basin[J].Geology and Exploration,2012,48(1):93-101.
[33] 唐鑫萍,黄文辉,邓宏文,等.山东平邑盆地古近系湖相微生物碳酸盐岩形成机理[J].古地理学报,2012,14(3):355-364.
TANG Xin-ping,HUANG Wen-hui,DENG Hong-wen,et al.Formation Mechanisms of the Paleogene Lacustrine Microbial Carbonate Rocks in Pingyi Basin,Shandong Province[J].Journal of Palaeogeography,2012,14(3):355-364.
[34] 张矿明,黄文辉,汪建辉,等.山东省平邑盆地古近系湖相核形石特征及环境意义[J].沉积学报,2013,31(2):259-268.
ZHANG Kuang-ming,HUANG Wen-hui,WANG Jian-hui,et al.Characteristics and Environmental Significance of Lacustrine Oncolites in Paleogene Guanzhuang Formation in Pingyi Basin,Shandong Province in Eastern China[J].Acta Sedimentologica Sinica,2013,31(2):259-268.
[35] 谢庆宾,管守锐,李熙哲.山东平邑盆地官中段沉积环境和层序地层特征[J].沉积学报,1999,17(1):71-78.
XIE Qing-bin,GUAN Shou-rui,LI Xi-zhe.Depositional Environmental and Sequence Stratigraphy Characte-ristics of Middle Member of the Guanzhong Formation in the Pingyi Basin,Shandong[J].Acta Sedimentologica Sinica,1999,17(1):71-78.
[36] 管守锐,白光勇,狄明信.山东平邑盆地下第三系官庄组中段碳酸盐岩沉积特征及沉积环境[J].华东石油学院学报,1985(3):9-20.
GUAN Shou-rui,BAI Guang-yong,DI Ming-xin.Sedi-mentary Characteristics and Environment of Carbonate Rocks in the Middle Member of the Guanzhuang Formation of Lower Tertiary in the Pingyi Basin of Shandong Province[J].Journal of East China Petroleum Institute,1985(3):9-20.
[37] 迟洪纪,何湘龙,王士林.山东平邑盆地下第三系的划分[J].地层学杂志,1986,10(2):121-127.
CHI Hong-ji,HE Xiang-long,WANG Shi-lin.Classification of the Stratigraphy of the Paleogene in the Pingyi Basin,Shandong[J].Journal of Stratigraphy,1986,10(2):121-127.
[38] 关绍曾,庞其清,萧宗正.鲁西南莱芜、蒙阴、平邑盆地早第三纪地层的划分和对比[J].化工矿产地质,1997,19(3):149-162.
GUAN Shao-zeng,PANG Qi-qing,XIAO Zong-zheng.Division and Correlation of Stratigraphy Among Early Tertiary Basins:Laiwu,Mengyin and Pingyi in Southwest Shandong[J].Geology of Chemical Minerals,1997,19(3):149-162.
[39] 张增奇,杜圣贤,张尚坤,等.山东平邑盆地官庄群有关地层的重新厘定[J].地层学杂志,2014,38(1):8-25.
ZHANG Zeng-qi,DU Sheng-xian,ZHANG Shang-kun,et al.Reassessment of the Guanzhuang Group in the Pingyi Basin,Shandong[J].Journal of Stratigraphy,2014,38(1):8-25.
[40] 杜圣贤,刘凤臣,陈 军,等.山东平邑盆地晚白垩世—古新世生物地层及白垩系/古近系界线研究[J].地质学报,2019,93(8):1831-1848.
DU Sheng-xian,LIU Feng-chen,CHEN Jun,et al.The Cretaceous-Paleocene Biostratigraphy and Boundary in the Pingyi Basin,Shandong Province[J].Acta Geologica Sinica,2019,93(8):1831-1848.
[41] 杜圣贤,李 越,宋香锁,等.山东平邑盆地卞桥组(晚白垩世马斯特里赫特晚期)泉华成因的核形石[J].微体古生物学报,2016,33(3):325-333.
DU Sheng-xian,LI Yue,SONG Xiang-suo,et al.Travertine-type Oncoids from the Cretaceous Bianqiao Formation(Late Maastrichtian)in the Pingyi Basin,Shandong Province,East China[J].Acta Micropalaeontologica Sinica,2016,33(3):325-333.
[42] 杜圣贤,王启飞,宋香锁,等.山东平邑盆地古新世孢粉组合及其古气候意义[J].微体古生物学报,2015,32(4):419-429.
DU Sheng-xian,WANG Qi-fei,SONG Xiang-suo,et al.Paleocene Sporo-pollen Fossils of the Pingyi Basin,Shandong Province,China[J].Acta Micropalaeontologica Sinica,2015,32(4):419-429.
[43] 唐鑫萍,黄文辉,邓宏文,等.山东平邑盆地古近系湖相核形石的沉积环境分析[J].现代地质,2011,25(3):456-463.
TANG Xin-ping,HUANG Wen-hui,DENG Hong-wen,et al.Sedimentary Environment of Paleogene Lacustrine Oncoids in Pingyi Basin,Shandong Province[J].Geoscience,2011,25(3):456-463.
[44] 于学峰,杜圣贤,王启飞,等.山东平邑盆地晚白垩世介形类[J].微体古生物学报,2014,31(4):387-404.
YU Xue-feng,DU Sheng-xian,WANG Qi-fei,et al.Late Cretaceous Ostracods from the Pingyi Basin,Shandong Province,China[J].Acta Micropalaeontologica Sinica,2014,31(4):387-404.
[45] 杜圣贤,卢辉楠,刘书才,等.山东平邑盆地晚白垩世孢粉化石[J].微体古生物学报,2013,30(4):379-388.
DU Sheng-xian,LU Hui-nan,LIU Shu-cai,et al.Late Cretaceous Sporo-pollen Fossils of the Pingyi Basin,Shandong Province[J].Acta Micropalaeontologica Sinica,2013,30(4):379-388.
[46] 杨景林,徐 健,刘凤臣,等.山东平邑盆地固城组和卞桥组的介形类动物群[J].微体古生物学报,2013,30(2):145-165.
YANG Jing-lin,XU Jian,LIU Feng-chen,et al.Ostracode Faunas from the Gucheng and Bianqiao Formations in Pingyi Basin,Shandong[J].Acta Micropalaeontologica Sinica,2013,30(2):145-165.
[47] 杜圣贤,于深洋,宋香锁,等.山东费县白垩纪末期卞桥组的湖相灰岩[J].微体古生物学报,2016,33(4):444-451.
DU Sheng-xian,YU Shen-yang,SONG Xiang-suo,et al.Lacustrine Limestones of the Bianqiao Formation(Maa-strichtian,Latest Cretaceous)from Feixian,Shandong Province,East China[J].Acta Micropalaeontologica Sinica,2016,33(4):444-451.
[48] 姜在兴.沉积学[M].北京:石油工业出版社,2003.
JIANG Zai-xing.Sedimentology[M].Beijing:Petroleum Industry Press,2003.
[49] SY/T 5238—2008,有机物和碳酸盐岩碳、氧同位素分析方法[S].
SY/T 5238—2008,Analysis Method for Carbon and Oxygen Isotope of Organic Matter and Carbonate[S].
[50] GB/T 14506.30—2010,硅酸盐岩石化学分析方法第30部分:44个元素量测定[S].
GB/T 14506.30—2010,Methods for Chemical Analysis of Silicate Rocks,Part 30:Determination of 44 Elements[S].
[51] KAUFMAN A J,JACOBSEN S B,KNOLL A H.The Vendian Record of Sr and C Isotopic Variations in Seawater:Implications for Tectonics and Paleoclimate[J].Earth and Planetary Science Letters,1993,120(3/4):409-430.
[52] 曹红霞,尚 婷,吴海燕,等.鄂尔多斯盆地东南部马家沟组碳酸盐岩碳氧同位素特征及意义[J].西北大学学报(自然科学版),2018,48(4):578-586.
CAO Hong-xia,SHANG Ting,WU Hai-yan,et al.Characteristics of Carbon and Oxygen Isotopes of Carbonate Rocks in Majiagou Formation and Their Implication,Southeastern Ordos Basin[J].Journal of Northwest University(Natural Science Edition),2018,48(4):578-586.
[53] 黄文辉,刘文中,BAUSCH W M.德国南部地区上侏罗统麻姆组碳酸盐岩碳、氧稳定同位素研究[J].地球化学,1999,28(1):97-102.
HUANG Wen-hui,LIU Wen-zhong,BAUSCH W M.Stable Isotopes(C,O)of Upper Jurassic Malm Carbonate Rocks in Southern Germany[J].Geochimica,1999,28(1):97-102.
[54] TALBOT M R.A Review of the Palaeohydrological Interpretation of Carbon and Oxygen Isotopic Ratios in Primary Lacustrine Carbonates[J].Chemical Geology:Isotope Geoscience Section,1990,80(4):261-279.
[55] 王春连,刘成林,徐海明,等.江陵凹陷古新世盐湖沉积碳酸盐碳氧同位素组成及其环境意义[J].地球学报,2013,34(5):567-576.
WANG Chun-lian,LIU Cheng-lin,XU Hai-ming,et al.Carbon and Oxygen Isotopes Characteristics of Palaeocene Saline Lake Facies Carbonates in Jiangling Depression and Their Environmental Significance[J].Acta Geoscientica Sinica,2013,34(5):567-576.
[56] MATHER C C,SKRZYPEK G,DOGRAMACI S,et al.Paleoenvironmental and Paleohydrochemical Conditions of Dolomite Formation Within a Saline Wetland in Arid Northwest Australia[J].Quaternary Science Reviews,2018,185:172-188.
[57] MARTIN-BELLO L,ARENAS C,ANDREWS J E,et al.Lacustrine Stromatolites as Multi-scale Recorders of Climate Change:Insights from the Miocene Ebro Basin[J].Palaeogeography,Paleoclimatology,Palaeoecology,2019,530:312-329.
[58] 马奂奂,刘池洋,张 龙,等.鄂尔多斯盆地延长组长7段沉积岩元素地球化学特征及沉积环境分析[J].现代地质,2019,33(4):872-882.
MA Huan-huan,LIU Chi-yang,ZHANG Long,et al.Geochemical Characteristics and Depositional Environment Implications of Sedimentary Rocks in the Chang-7 Member of Yanchang Formation in the Ordos Basin[J].Geoscience,2019,33(4):872-882.
[59] 逄淑伊,操应长,梁 超.渤海湾盆地东营凹陷沙四上亚段—沙三下亚段岩相特征及沉积环境:以樊页1井为例[J].石油与天然气地质,2019,40(4):799-809.
PANG Shu-yi,CAO Ying-chang,LIANG Chao.Lithofacies Characteristics and Sedimentary Environment of EsU4 and EsL3:A Case Study of Well FY1 in Dongying Sag,Bohai Bay Basin[J].Oil and Gas Geology,2019,40(4):799-809.
[60] 王 卓,赵靖舟,陈宇航.鄂东神府地区山西组古沉积环境及沉积特征分析[J].西安石油大学学报(自然科学版),2019,34(5):24-30,36.
WANG Zhuo,ZHAO Jing-zhou,CHEN Yu-hang.Analysis of Palaeo-sedimentary Environment and Characteristics of Shanxi Formation in Shenfu Area on the Eastern Margin of Ordos Basin[J].Journal of Xi'an Shi-you University(Natural Science Edition),2019,34(5):24-30,36.
[61] KELTS K,TALBOT M.Lacustrine Carbonates as Geo-chemical Archives of Environmental Change and Biotic/Abiotic Interactions[M].Berlin:Springer,1990.
[62] 刘成东,刘 友,万建军,等.衢州市上方镇方解石矿床碳、氧同位素地球化学特征[J].矿物岩石地球化学通报,2019,38(2):374-378,394.
LIU Cheng-dong,LIU You,WAN Jian-jun,et al.Carbon and Oxygen Isotopic Composition of the Shangfang Calcite Deposit in Quzhou City,Zhejiang Province[J].Bulletin of Mineralogy,Petrology and Geochemistry,2019,38(2):374-378,394.
[63] 徐崇凯,刘池洋,郭 佩,等.潜江凹陷古近系潜江组盐间泥岩地球化学特征及地质意义[J].沉积学报,2018,36(3):617-629.
XU Chong-kai,LIU Chi-yang,GUO Pei,et al.Geochemical Characteristics and Their Geological Significance of Intrasalt Mudstones from the Paleogene Qianjiang Formation in the Qianjiang Graben,Jianghan Basin,China[J].Acta Sedimentologica Sinica,2018,36(3):617-629.
[64] 王随继,黄杏珍,妥进才,等.泌阳凹陷核桃园组微量元素演化特征及其古气候意义[J].沉积学报,1997,15(1):65-70.
WANG Sui-ji,HUANG Xing-zhen,TUO Jin-cai,et al.Evolutional Characteristics and Their Paleoclimate Significance of Trace Elements in the Hetaoyuan Formation,Biyang Depression[J].Acta Sedimentologica Sinica,1997,15(1):65-70.

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Last Update: 2020-05-27