鲁西地区含白云石碳酸盐岩的矿物学特征及其形成环境分析-岩石矿物学杂志-CSCIED科技核心评价数据库-手机版

鲁西地区含白云石碳酸盐岩的矿物学特征及其形成环境分析

Analysis of mineralogical characteristics and formation environment of dolomitic carbonate rocks in western Shandong

ES评分 0 浏览量：236 下载量：0

DOI	10.20086/j.cnki.yskw.2023.0304
刊名	岩石矿物学杂志 Acta Petrologica et Mineralogica
年，卷(期)	2023, 42(3)
作者	章源隆，周川野，黎晏彰，鲁安怀*，丁竑瑞，王长秋，李艳,
作者单位	造山带与地壳演化教育部重点实验室, 矿物环境功能北京市重点实验室, 北京大学地球与空间科学学院, 北京 100871
摘要	白云石的成因受到地质学界的广泛关注,现今在实验室中能够利用微生物合成高有序度的白云石,但天然白云石的成因与原始沉积环境特征的相关性并未完全揭示。本研究选取鲁西地区馒头组含白云石碳酸盐岩沉积地层为研究对象,通过矿物学、元素地球化学等分析,初步判断该地层白云石成因并重建白云石地层的古沉积环境,探讨了两者之间的关系。结果表明:白云石含量在本套地层中的均值为52.45%。Sr/Cu值(均值为23.59)与Ga/Rb值(均值为0.17)指示其整体表现为炎热干旱的古气候特征。δ¹³C值(均值为-1.56‰)与δ¹⁸O值(均值为-6.68‰)指示本套地层为海相沉积,推测古水温平均为23.5℃,古氧化还原特征表现为弱还原至常氧化的平稳过渡。灰岩地层δ¹³C值平均为-0.80‰,而白云岩地层δ¹³C值平均为-6.52‰,存在轻碳的明显富集,结合宏观叠层构造,判断白云石为生物成因。本研究中白云石沉积环境中的古气候、古氧化还原条件、古水温和古生产力特征与白云石发育情况存在明显耦合,为白云石生物成因提供了相关依据与指示意义。
Abstract	The origin of dolomite has been widely concerned by the geologists. Nowadays, microorganisms can be used to synthesize dolomite with high order in the laboratory, but the correlation between the origin of natural dolomite and the characteristics of the original sedimentary environment has yet to be fully revealed. In this study, the dolomitic carbonate sedimentary strata of Mantou Formation in western Shandong Province are selected as the research object. Through the analysis of mineralogy element geochemistry, the origin of dolomite in this formation is preliminarily judged and the paleosedimentary environment of dolomite formation is reconstructed. The relationship between them is discussed. The semiquantitative results show that the average content of dolomite in this set of strata is 52.45%. The ratio of Sr/Cu (mean value is 23.59) and Ga/Rb (mean value is 0.17) indicates that it is characterized by hot and arid paleoclimate. δ¹³C (mean value is -1.56‰) and δ¹⁸O (mean value is -6.68‰) indicate that this set of strata is marine sedimentation, and it is speculated that the average paleotemperature is 23.5℃. Furthermore, the paleoredox features a smooth transition from weak reduction to oxidation. The mean value of δ¹³C in the limestone stratum is -0.80‰, while that in the dolomite stratum is -6.52‰. The pronounced enrichment of light carbon in the sample and the combination of macro stack structure indicate that dolomite is of biological origin. In this study, the characteristics of paleoclimate, paleoredox conditions, paleotemperature and paleoproductivity in the dolomite sedimentary environment are obviously coupled with dolomite development, providing a relevant basis and indicating significance for dolomite biogenesis.
关键词	白云石成因；鲁西地区；矿物学；地球化学；古沉积环境
KeyWord	origin of dolomite; western Shandong; mineralogy; geochemistry; paleosedimentary environment
基金项目
页码	365-378

参考文献
相关文献

Adams J E and Rhodes M L. 1960. Dolomitization by seepage refluxion
[J]. AAPG Bulletin, 44(12): 1 912~1 920. Bai S L. 1994. Devonian Events and Biostratigraphy of South China
[M]. Beijing: Peking University Press. Beckmann B, Flögel S, Hofmann P, et al. 2005. Orbital forcing of Cretaceous river discharge in tropical Africa and ocean response
[J]. Nature, 437(7 056): 241~244. Cao J, Wu M, Chen Y, et al. 2012. Trace and rare earth element geochemistry of Jurassic mudstones in the northern Qaidam Basin, northwest China
[J]. Geochemistry, 72(3): 245~252. Chen Jinbiao, Wu Tieshan, Zhang Pengyuan, et al. 1997. Regional Stratigraphy in North China—— Study on Multiple Stratigraphic Division and Correlation in China
[M]. Wuhan: China University of Geosciences Press(in Chinese). Ding J, Zhang J, Tang X, et al. 2018. Elemental geochemical evidence for depositional conditions and organic matter enrichment of black rock series strata in an inter-platform basin: The Lower Carboniferous Datang Formation, Southern Guizhou, Southwest China
[J]. Minerals, 8(11): 509. Dymond J, Suess E and Lyle M. 1992. Barium in deep-sea sediment: A geochemical proxy for paleoproductivity
[J]. Paleoceanography, 7(2): 163~181. Feng Zengzhao, Chen Jixin and Wu Shenghe. 1989. Early Paleozoic lithofacies palaeogeography of North China platform
[J]. Acta Sedimentologica Sinica, 7 (4): 15~55(in Chinese with English abstract). Francois R, Honjo S, Manganini S J, et al. 1995. Biogenic barium fluxes to the deep sea: Implications for paleoproductivity reconstruction
[J]. Global Biogeochemical Cycles, 9(2): 289~303. Han S, Zhang Y, Huang J, et al. 2020. Elemental geochemical characterization of sedimentary conditions and organic matter enrichment for lower cambrian shale formations in northern guizhou, south China
[J]. Minerals, 10(9): 793. Han Z, Zhang X, Chi N, et al. 2015. Cambrian oncoids and other microbial-related grains on the North China Platform
[J]. Carbonates and Evaporites, 30(4): 373~386. Hatch J and Leventhal J. 1992. Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian (Missourian) Stark Shale Member of the Dennis Limestone, Wabaunsee County, Kansas, USA
[J]. Chemical Geology, 99(1~3): 65~82. Huang Jiqing. 1954. Characteristics of regional geology in China
[J]. Acta Geologica Sinica, 34 (3): 217~244(in Chinese with English abstract). Jin Zhenkui, Shi Liang, Gao Baishui, et al. 2013. Carbonate facies and facies models
[J]. Acta Sedimentologica Sinica, 31(6): 965~979(in Chinese with English abstract). Jones B and Manning D A. 1994. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones
[J]. Chemical Geology, 111(1~4): 111~129. Keith M and Weber J. 1964. Carbon and oxygen isotopic composition of selected limestones and fossils
[J]. Geochimica et Cosmochimica Acta, 28(10~11): 1 787~1 816. Latif K, Xiao E, Riaz M, et al. 2019. Calcified cyanobacteria fossils from the leiolitic bioherm in the Furongian Changshan Formation, Datong (North China Platform)
[J]. Carbonates and Evaporites, 34(3): 825~843. Liu Benpei, Quan Qiuqi, Feng Qinglai, et al. 1996. Geohistory Course
[M]. Beijing: Geological Publishing House(in Chinese). Liu Lihong, Gao Yongjin, Wang Dandan, et al. 2021. The impact of gypsum salt rock on Cambrian subsalt dolomite reservoir in Tarim Basin
[J]. Acta Petrologica et Mineralogica, 40(1): 109~120(in Chinese with English abstract). Lu P and Cantrell D. 2016. Reactive transport modelling of reflux dolomitization in the Arab-D reservoir, Ghawar field, Saudi Arabia
[J]. Sedimentology, 63(4): 865~892. Machel H G and Lonnee J. 2002. Hydrothermal dolomite—A product of poor definition and imagination
[J]. Sedimentary Geology, 152(3~4): 163~171. McKenzie J A. 1985. Carbon isotopes and productivity in the lacustrine and marine environment
[C]// Stumm W. Chemical Processes in Lakes. Wiley: New York, 99~118. Rivers J M, Kurt K T and James N P. 2012. Salinity reflux and dolomitization of southern Australian slope sediments: The importance of low carbonate saturation levels
[J]. Sedimentology, 59(2): 445~465. Roy D K and Roser B P. 2013. Climatic control on the composition of Carboniferous-Permian Gondwana sediments, Khalaspir basin, Bangladesh
[J]. Gondwana Research, 23(3): 1 163~1 171. Shao Longyi. 1994. Relationship between oxygen and carbon isotopes of carbonate rocks and paleotemperature
[J]. Journal of China University of Mining & Technology, 23(1): 39~45(in Chinese with English abstract). Shields G and Stille P. 2001. Diagenetic constraints on the use of cerium anomalies as palaeoseawater redox proxies: An isotopic and REE study of Cambrian phosphorites
[J]. Chemical Geology, 175(1~2): 29~48. Smith Jr L B and Davies G R. 2006. Structurally controlled hydrothermal alteration of carbonate reservoirs: Introduction
[J]. AAPG Bulletin, 90(11): 1 635~1 640. Song Mingchun, Li Peiyuan, Xiong Yuxin, et al. 2008. Deep iron deposit of the Jining intense magnetic anomaly area in Shandong Province and its significance
[J]. Acta Geologica Sinica, 82(9): 1 285~1 291(in Chinese with English abstract). Tribovillard N, Algeo T J, Lyons T, et al. 2006. Trace metals as paleoredox and paleoproductivity proxies: An update
[J]. Chemical Geology, 232(1~2): 12~32. Vasconcelos C and McKenzie J A. 1997. Microbial mediation of modern dolomite precipitation and diagenesis under anoxic conditions (Lagoa Vermelha, Rio de Janeiro, Brazil)
[J]. Journal of Sedimentary Research, 67(3): 378~390. Vasconcelos C, McKenzie J A, Bernasconi S, et al. 1995. Microbial mediation as a possible mechanism for natural dolomite formation at low temperatures
[J]. Nature, 377(6 546): 220~222. Wang Chunlian, Liu Chenglin, Xu Haiming, et al. 2013. Carbon and oxygen isotopes characteristics of Paleocene saline lake facies carbonates in Jiangling depression and their environmental significance
[J]. Acta Geoscientica Sinica, 34 (5): 567~576(in Chinese with English abstract). Wang Quan. 2011. North China Craton and global tectonics
[J]. Geological Bulletin of China, 30(1): 1~18(in Chinese with English abstract). Warthmann R, van Lith Y, Vasconcelos C, et al. 2000. Bacterially induced dolomite precipitation in anoxic culture experiments
[J]. Geology, 28(12): 1 091~1 094. Wright D T. 1999. The role of sulphate-reducing bacteria and cyanobacteria in dolomite formation in distal ephemeral lakes of the Coorong region, South Australia
[J]. Sedimentary Geology, 126(1~4): 147~157. Xie G, Shen Y, Liu S, et al. 2018. Trace and rare earth element (REE) characteristics of mudstones from Eocene Pinghu Formation and Oligocene Huagang Formation in Xihu Sag, East China Sea Basin: Implications for provenance, depositional conditions and paleoclimate
[J]. Marine and Petroleum Geology, 92: 20~36. Xin Hao, Xiao Enzhao, Qin Yinglun, et al. 2019. Sedimentary characteristics of large columnar stromatolites in Fengshan Formation of Xianrendong section of western Shandong area
[J]. Journal of Northeast Petroleum University, 43(3): 1~12(in Chinese with English abstract). Yandoka B M S, Abdullah W H, Abubakar M, et al. 2015. Geochemical characterisation of Early Cretaceous lacustrine sediments of Bima Formation, Yola Sub-basin, Northern Benue Trough, NE Nigeria: Organic matter input, preservation, paleoenvironment and palaeoclimatic conditions
[J]. Marine and Petroleum Geology, 61: 82~94. Yang Hucheng, Lin Liangbiao, Yu Yu, et al. 2022. Geochemical characteristics and paleoenvironmental significance of Middle Permian carbonate rocks in Tianquan area, southwestern Sichuan Province, China
[J]. Mineralogy and Petrology, 42(2): 47~59(in Chinese with English abstract). Yi Haisheng, Lin Jinhui, Zhou Kenken, et al. 2007. Carbon and oxygen isotope characteristics and paleoenvironmental implication of the Cenozoic lacustrine carbonate rocks in northern Qinghai-Tibet Plateau
[J]. Journal of Paleogeography, 9(3): 303~312(in Chinese with English abstract). You Xuelian, Sun Shu, Zhu Jingquan, et al. 2011. Progress in the study of microbial dolomite model
[J]. Earth Science Frontiers, 18(4): 52~64(in Chinese with English abstract). Zenger D H, Dunham J B and Ethington R L. 1980. Concepts and models of dolomitization: Based on a symposium sponsored by the Society of Economic Paleontologists and Mineralogists
[M]. The Society. Zhang Chunyu, Guan Shuwei, Wu Lin, et al. 2021. Geochemical characteristics and its paleoenvironmental significance of the lower Cambrian carbonate in the northwestern Tarim Basin: A case study of well Shutan-1
[J]. Bulletin of Geological Science and Technology, 40(5): 99~111(in Chinese with English abstract). Zhao Dongfang, Tan Xiucheng, Luo Bing, et al. 2022. A review of microbial dolomite: Advances and challenges
[J]. Acta Sedimentologica Sinica, 40(2): 335~349(in Chinese with English abstract). 陈晋镳, 武铁山, 张鹏远, 等. 1997. 华北区区域地层——全国地层多重划分对比研究
[M]. 武汉: 中国地质大学出版社. 冯增昭, 陈继新, 吴胜和. 1989. 华北地台早古生代岩相古地理
[J]. 沉积学报, 7(4): 15~55. 黄汲清. 1954. 中国区域地质的特征
[J]. 地质学报, 34(3): 217~229. 金振奎, 石良, 高白水, 等. 2013. 碳酸盐岩沉积相及相模式
[J]. 沉积学报, 31(6): 965~979. 刘本培, 全秋琦, 冯庆来, 等. 1996. 地史学教程
[M]. 北京: 地质出版社. 刘丽红, 高永进, 王丹丹, 等. 2021. 塔里木盆地寒武系膏盐岩对盐下白云岩储层的影响
[J]. 岩石矿物学杂志, 40(1): 109~120. 邵龙义. 1994. 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, 23(1): 39~45. 宋明春, 李培远, 熊玉新, 等 . 2008. 山东省济宁强磁异常区深部铁矿初步验证及其意义
[J]. 地质学报, 82(9): 1 285~1 291. 王春连, 刘成林, 徐海明, 等. 2013. 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, 34(5): 567~576. 王荃. 2011. 华北克拉通与全球构造
[J]. 地质通报, 30(1): 1~18. 辛浩, 肖恩照, 覃英伦, 等. 2019. 鲁西地区仙人洞剖面凤山组大型柱状叠层石沉积特征
[J]. 东北石油大学学报, 43(3): 1~11. 杨虎城, 林良彪, 余瑜, 等. 2022. 川西南天全地区中二叠统碳酸盐岩地球化学特征及其古环境意义
[J]. 矿物岩石, 42(2): 1~18. 伊海生, 林金辉, 周恳恳, 等. 2007. 青藏高原北部新生代湖相碳酸盐岩碳氧同位素特征及古环境意义
[J]. 古地理学报, 9(3): 303~312. 由雪莲, 孙枢, 朱井泉, 等. 2011. 微生物白云岩模式研究进展
[J]. 地学前缘, 18(4): 52~64. 张春宇, 管树巍, 吴林, 等. 2021. 塔西北地区下寒武统碳酸盐岩地球化学特征及其古环境意义: 以舒探 1 井为例
[J]. 地质科技通报, 40(5): 99~111. 赵东方, 谭秀成, 罗冰, 等. 2022. 微生物诱导白云石沉淀研究进展及面临的挑战
[J]. 沉积学报, 40(2): 335~349.

引用本文

章源隆，周川野，黎晏彰，鲁安怀*，丁竑瑞，王长秋，李艳. 鲁西地区含白云石碳酸盐岩的矿物学特征及其形成环境分析 [J]. 岩石矿物学杂志. 2023; 42; (3). 365 - 378.

文献评论

相关学者

相关机构