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碳酸盐工厂的精细刻画:定量化重建视角

王夏 孟令赞 柳晶晶 甯濛 葛毓柱 曾雨涵 李飞 颜佳新

沉积学报2024,Vol.42Issue(2):350-370,21.
沉积学报2024,Vol.42Issue(2):350-370,21.DOI:10.14027/j.issn.1000-0550.2024.047

碳酸盐工厂的精细刻画:定量化重建视角

Detailed Characterization of Carbonate Factories from the Perspective of Quantitative Reconstruction

王夏 1孟令赞 2柳晶晶 2甯濛 3葛毓柱 3曾雨涵 2李飞 4颜佳新5

作者信息

  • 1. 成都理工大学沉积地质研究院,成都 610059||油气藏地质及开发工程全国重点实验室,成都理工大学,成都 610059||国家能源碳酸盐岩油气重点实验室成都理工大学研究分室,成都理工大学,成都 610059||自然资源部深时地理环境重建与应用重点实验室,成都理工大学,成都 610059||自然资源部沉积盆地与油气资源重点实验室,成都 610218
  • 2. 成都理工大学沉积地质研究院,成都 610059
  • 3. 成都理工大学沉积地质研究院,成都 610059||油气藏地质及开发工程全国重点实验室,成都理工大学,成都 610059||国家能源碳酸盐岩油气重点实验室成都理工大学研究分室,成都理工大学,成都 610059||自然资源部深时地理环境重建与应用重点实验室,成都理工大学,成都 610059
  • 4. 天然气地质四川省重点实验室,西南石油大学地球科学与技术学院,成都 610500
  • 5. 生物地质与环境地质国家重点实验室,中国地质大学(武汉)地球科学学院,武汉 430074
  • 折叠

摘要

Abstract

[Significance]Carbonate factories provide the foundation for forming carbonate depositional systems.They are closely related to marine evolution,elemental cycling,and earth surface processes and are an essential part reflecting the evolution of the Earth system.The transition of carbonate factories often coincides with biological and environmental changes.Over geological time,the change of carbonate factories frequently occurs along with biologi-cal or environmental crises such as mass extinction or the initiation of new life forms such as life explosion or biologi-cal recovery after crisis.Therefore,quantifying the characterization of carbonate factories and their controlling factors is for a deeper understanding of the geological information recorded in carbonate rocks.[Progress]However,most studies on carbonate factories,particularly those from the geological records,are qualitative based on the lithological and microfacies analysis.This study summarizes the research progress in the semi-quantitative to quantitative charac-terization of carbonate factories,combining the introduction of the methods for forward modelling of sedimentary pro-cesses to provide a perspective for the detailed characterization of carbonate factories from a quantitative reconstruc-tion perspective.In addition to providing information on rock components that indicate the ingredients of carbonate factories,statistical analysis of carbonate grains can offer insights into the sedimentary environment by examining pa-rameters such as size,roundness,and sorting.These shape characteristics can serve as quantitative indicators of wa-ter energy and grain transportation processes.Elemental geochemical proxies enable the assessment of environmental parameters such as redox conditions,nutrient levels,and climatic conditions.Isotopic geochemical proxies play a crucial role in reconstructing the evolution of environmental factors such as temperature and seawater carbonate satu-ration.By a combination of multiproxies and sedimentary process modelling,a comprehensive analysis can identify the production process,controlling factors,and evolution of carbonate factories.[Prospects]Based on traditional carbonate sedimentology,studying carbonate factories should deepen our understanding of their controlling factors,particularly the quantitative assessment of factors directly impacting ecosystems.When applying quantitative analysis methods such as sediment transport patterns or hydrodynamic analysis that are established in siliciclastic sedimentary systems,the differences caused by the biogenic nature of certain carbonate sediments compared to siliciclastic sediments need to be considered.Furthermore,models and analysis methods applicable to carbonate grains should be further refined.In addition,when quantitatively evaluating the development of carbonate factories in ancient marine using quantitative carbonate grains statistics or geochemical indicators,there should be a strengthened focus on developing quantitative assessment methods for the level of diagenetic alteration.Further efforts should be directed toward developing and applying in-situ elemental and isotopic testing methods to reduce the impact of diagenesis on geochemical signals.While developing and applying new geochemical proxies for carbonate rocks,the mechanisms of occurrence or fractionation need to be clearly understood to interpret the reflected paleoclimate and paleoenvironmental information accurately.Simultaneously,when studying deep-time evolution and production mecha-nisms of carbonate factories through sedimentary process forward modelling,it is necessary to consider the applicability of parameters obtained from modern environments in deep-time records and account for the impact of syndepositional-early diagenesis and chemical evolution of seawater geochemical evolution in the modelling process.

关键词

碳酸盐工厂/定量分析/碳酸盐颗粒/元素地球化学/同位素地球化学/地层正演模拟

Key words

carbonate factory/quantitative analysis/carbonate grains/element geochemistry/isotope geochemistry/stratigraphic forward modelling

分类

天文与地球科学

引用本文复制引用

王夏,孟令赞,柳晶晶,甯濛,葛毓柱,曾雨涵,李飞,颜佳新..碳酸盐工厂的精细刻画:定量化重建视角[J].沉积学报,2024,42(2):350-370,21.

基金项目

国家自然科学基金项目(42102143,42272131,42293291) (42102143,42272131,42293291)

自然资源部沉积盆地与油气资源重点实验室开放基金(cdcgs2022003) National Natural Science Foundation of China,No.42102143,42272131,42293291 (cdcgs2022003)

Open Foundation of Key Laboratory of Sedimentary Basin and Oil and Gas Resources,Ministry of Natural Resources,No.cdcgs2022003 ()

沉积学报

OA北大核心CSTPCD

1000-0550

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