Skip to main content
Log in

Constraints of palaeoenvironment on organic matter of Benxi Formation shale and discussion on enrichment mechanism under different facies

  • Research Article
  • Published:
Frontiers of Earth Science Aims and scope Submit manuscript

Abstract

As a hydrocarbon-rich sedimentary basin in China, the Ordos Basin has enormous potential for shale gas resources. The shale of the Upper Carboniferous Benxi Formation is rich in organic matter, however, its palaeoenvironment and organic matter enrichment mode are yet to be revealed. In this study, the geochemical characteristics of the shale of the Benxi Formation in the east-central part of the Ordos Basin were analyzed to investigate its palaeoenvironment. At the same time, the organic matter enrichment modes in different sedimentary facies were compared and analyzed. The results indicate that: 1) the shale of the Benxi Formation was mainly deposited on the continental margin and strong terrestrial clastic input; 2) the deposition period of the Benxi Formation shale had a hot and humid climate with high palaeoproductivity and local volcanic hydrothermal fluid, and a high sedimentation rate with the strong stagnant environment. The bottom water was in dysoxic conditions and a semi-saline deposition environment; 3) multiple factors, such as palaeoproductivity, volcanic hydrothermal, redox conditions, and palaeosalinity interact to influence the enrichment of shale organic matter in Benxi Formation; 4) the organic matter enrichment modes of continental, marine-continental transitional, and marine shales can be classified into three types: “production mode”, “hybrid mode of preservation and production”, and “preservation mode”, respectively. This study provides a reference for the organic matter enrichment mode, shale gas formation conditions, and core area evaluation in these marine-continental transitional shales, and also offers new guidance for exploration ideas for shale gas in different sedimentary facies.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Abanda P A, Hannigan R E (2006). Effect of diagenesis on trace element partitioning in shales. Chem Geol, 230(1–2): 42–59

    Article  Google Scholar 

  • Algeo T J, Rowe H (2012). Paleoceanographic applications of trace-metal concentration data. Chem Geol, 324–325: 6–18

    Article  Google Scholar 

  • Algeo T J, Tribovillard N (2009). Environmental analysis of paleoceanographic systems based on molybdenum-uranium covariation. Chem Geol, 268(3–4): 211–225

    Article  Google Scholar 

  • Awan R S, Liu C, Gong H, Dun C, Tong C, Chamssidini L G (2020). Paleo-sedimentary environment in relation to enrichment of organic matter of Early Cambrian black rocks of Niutitang Formation from Xiangxi area China. Mar Pet Geol, 112: 104057

    Article  Google Scholar 

  • Bernárdez P, Gonzalez-Alvarez R, Frances G, Prego R, Barcena M A, Romero O E (2008). Late Holocene history of the rainfall in the NW Iberian peninsula - evidence from a marine record. J Mar Syst, 72(1–4): 366–382

    Article  Google Scholar 

  • Chen Y, Liu S, Zhu Z, Wang Z, Sun X, Xu T (2021). Geochemical characteristics and sedimentary setting of chang 9 shale in the Upper Triassic Yanchang Formation of southeastern Ordos Basin (NW China). J Petrol Sci Eng, 196: 108081

    Article  Google Scholar 

  • Chen Y, Wang Y, Guo M, Wu H, Li J, Wu W, Zhao J (2020). Differential enrichment mechanism of organic matters in the marine-continental transitional shale in northeastern Ordos Basin, China: control of sedimentary environments. J Nat Gas Sci Eng, 83: 103625

    Article  Google Scholar 

  • Chen Y, Zhu Z, Zhang L (2019). Control actions of sedimentary environments and sedimentation rates on lacustrine oil shale distribution, an example of the oil shale in the Upper Triassic Yanchang Formation, southeastern Ordos Basin (NW China). Mar Pet Geol, 102: 508–520

    Article  Google Scholar 

  • Cui C, Zhang H, Liu W, Li S, Liu Y, Song H, Wu C M, Wen Z (2022). Element geochemical characteristics of shale in the first member of Benxi Formation in eastern Ordos Basin: take Zhaoxian section and M115 well in Linxian County, Shanxi as examples. Nat Gas Geosci, 33(6): 1001–1012 (in Chinese)

    Google Scholar 

  • Cullers R L, Podkovyrov V N (2002). The source and origin of terrigenous sedimentary rocks in the Mesoproterozoic Ui group, southeastern Russia. Precambrian Res, 117(3–4): 157–183

    Article  Google Scholar 

  • Ding W, Zhu D, Cai J, Gong M, Chen F (2013). Analysis of the developmental characteristics and major regulating factors of fractures in marine-continental transitional shale-gas reservoirs: a case study of the Carboniferous-Permian strata in the southeastern Ordos Basin, central China. Mar Pet Geol, 45: 121–133

    Article  Google Scholar 

  • Ding X, Liu G, Zha M, Huang Z, Gao C, Lu X, Sun M, Chen Z, Liuzhuang X (2015). Relationship between total organic carbon content and sedimentation rate in ancient lacustrine sediments, a case study of Erlian basin, northern China. J Geochem Explor, 149: 22–29

    Article  Google Scholar 

  • Doner Z, Kumral M, Demirel I H, Hu Q (2019). Geochemical characteristics of the Silurian shales from the central Taurides, southern Turkey: organic matter accumulation, preservation and depositional environment modeling. Mar Pet Geol, 102: 155–175

    Article  Google Scholar 

  • Dong Z, Zhang J, Tang X, Liu G, Dang W, Liu Y, Tao J, Su Z (2020). Origin and diffusion of the over-mature transitional natural gas in multiple lithologic reservoirs: a case study of Carboniferous-Permian strata in the southeastern margin of Ordos Basin. Int J Coal Geol, 219: 103380

    Article  Google Scholar 

  • Dypvik H, Harris N B (2001). Geochemical facies analysis of finegrained siliciclastics using Th/U, Zr/Rb and (Zr+Rb)/Sr ratios. Chem Geol, 181(1–4): 131–146

    Article  Google Scholar 

  • Elderfield H, Greaves M J (1982). The rare earth elements in seawater. Nature, 296(5854): 214–219

    Article  Google Scholar 

  • Fedo C M, Wayne Nesbitt H, Young G M (1995). Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance. Geology, 23(10): 921–924

    Article  Google Scholar 

  • Floyd P A, Leveridge B E (1987). Tectonic environment of the Devonian Gramscatho basin, south Cornwall: framework mode and geochemical evidence from turbiditic sandstones. J Geol Soc London, 144(4): 531–542

    Article  Google Scholar 

  • Guo H (2020). Study on the Mechanism and Controlling Factors of Shale Gas Enrichment in Shanxi Formation-a Case Study of the Eastern Ordos Basin. Dissertation for Master Degree. Xi’an Shiyou University (in Chinese)

  • Haskin L A, Haskin M A, Frey F A, Wildeman T R (1968). Relative and absolute terrestrial abundances of the rare earths. In: Ahrens L H, ed. Origin Distribution of the Elements. Elsevier, 889–912

  • Hatch J R, Leventhal J S (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, U.S.A. Chem Geol, 99(1–3): 65–82

    Article  Google Scholar 

  • He Q, Li D, Sun Q, Wei B, Wang S (2022). Main controlling factors of marine shale compressive strength: a case study on the Cambrian Niutitang Formation in Dabashan Mountain. Energy, 260: 125100

    Article  Google Scholar 

  • He T, Lu S, Li W, Tan Z, Zhang X (2018). Effect of salinity on source rock formation and its control on the oil content in shales in the Hetaoyuan Formation from the Biyang Depression, Nanxiang Basin, Central China. Energy Fuels, 32(6): 6698–6707

    Article  Google Scholar 

  • Hoyle J, Elderfield H, Gledhill A, Greaves M (1984). The behaviour of the rare earth elements during mixing of river and sea waters. Geochim Cosmochim Acta, 48(1): 143–149

    Article  Google Scholar 

  • Hu T, Pang X, Jiang S, Wang Q, Xu T, Lu K, Huang C, Chen Y, Zheng X (2018). Impact of paleosalinity, dilution, redox, and paleoproductivity on organic matter enrichment in a saline lacustrine rift basin: a case study of paleogene organic-rich shale in Dongpu Depression, Bohai Bay Basin, eastern China. Energy Fuels, 32(4): 5045–5061

    Article  Google Scholar 

  • Hu Y, Liu Y, Guo Y, Liu W, Zhang Z, Yang X (2022). Elemental geochemical characteristics of mudstones in Upper Carboniferous Benxi Formationin southern Ordos Basin and their enlightenment to sedimentary environment. J Shandong U Sci Techn (Nat Sci), 41: 13–23

    Google Scholar 

  • Jenkyns H C, Dickson A J, Ruhl M, Boorn S H J M (2017). Basaltseawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian-Turonian, Late Cretaceous). Sedimentology, 64(1): 16–43

    Article  Google Scholar 

  • Jones B, Manning D A C (1994). Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones. Chem Geol, 111(1–4): 111–129

    Article  Google Scholar 

  • Khaled A, Li R, Xi S, Zhao B, Wu X, Yu Q, Zhang Y, Li D (2022). Paleoenvironmental conditions and organic matter enrichment of the Late Paleoproterozoic Cuizhuang Formation dark shale in the Yuncheng Basin, north China. J Petrol Sci Eng, 208: 109627

    Article  Google Scholar 

  • Lan Z, Shen J (2022). Depositional Paleo-environments of Lower Cambrian Qiongzhusi Formation in the western middle Yangtze Block and its controlling effect on the organic matter enrichment. Energies, 15(10): 3761

    Article  Google Scholar 

  • Latimer J C, Filippelli G M (2002). Eocene to Miocene terrigenous inputs and export production: geochemical evidence from ODP Leg 177, Site 1090. Palaeogeogr Palaeoclimatol Palaeoecol, 182(3–4): 151–164

    Article  Google Scholar 

  • Li D, Li R, Tan C, Zhao D, Xue T, Zhao B, Khaled A, Liu F, Xu F (2019a). Origin of silica, paleoenvironment, and organic matter enrichment in the Lower Paleozoic Niutitang and Longmaxi formations of the northwestern Upper Yangtze Plate: significance for hydrocarbon exploration. Mar Pet Geol, 103: 404–421

    Article  Google Scholar 

  • Li W, Li J, Lu S, Chen G, Pang X, Zhang P, He T (2022). Evaluation of gas-in-place content and gas-adsorbed ratio using carbon isotope fractionation model: a case study from Longmaxi shales in Sichuan Basin, China. Int J Coal Geol, 249: 103881

    Article  Google Scholar 

  • Li W, Zhang Q, Li K, Chen Q, Guo Y, Ma Y, Feng J, Zhang D (2021). Sedimentary evolution of the late Paleozoic in Ordos Basin and its adjacent areas. J Palaeogeogr, 23: 39–52 (in Chinese)

    Google Scholar 

  • Li X, Gang W, Yao J, Gao G, Wang C, Li J, Liu Y, Guo Y, Yang S (2020). Major and trace elements as indicators for organic matter enrichment of marine carbonate rocks: a case study of Ordovician subsalt marine formations in the central-eastern Ordos Basin, north China. Mar Pet Geol, 111: 461–475

    Article  Google Scholar 

  • Li Y, Gao X, Meng S, Wu P, Niu X, Qiao P, Elsworth D (2019c). Diagenetic sequences of continuously deposited tight sandstones in various environments: a case study from upper Paleozoic sandstones in the Linxing area, eastern Ordos basin, China. AAPG Bull, 103(11): 2757–2783

    Article  Google Scholar 

  • Li Y, Wang Z, Gan Q, Niu X, Xu W (2019b). Paleoenvironmental conditions and organic matter accumulation in Upper Paleozoic organic-rich rocks in the east margin of the Ordos Basin, China. Fuel, 252: 172–187

    Article  Google Scholar 

  • Liang J, Tao W, Ma X (2020). Origin and paleoenvironmental reconstruction of phosphorus-bearing sandstones of the Cambrian Xinji Formation, southwestern margin of the Ordos Basin, China. Can J Earth Sci, 57(8): 903–917

    Article  Google Scholar 

  • Liu S, Wu C, Li T, Wang H (2018). Multiple geochemical proxies controlling the organic matter accumulation of the marine-continental transitional shale: a case study of the Upper Permian Longtan Formation, western Guizhou, China. J Nat Gas Sci Eng, 56: 152–165

    Article  Google Scholar 

  • Ma Y, Lu Y, Liu X, Zhai G, Wang Y, Zhang C (2019). Depositional environment and organic matter enrichment of the lower Cambrian Niutitang shale in western Hubei Province, South China. Mar Pet Geol, 109: 381–393

    Article  Google Scholar 

  • McLennan S M (2001). Relationships between the trace element composition of sedimentary rocks and upper continental crust. Geochem Geophys Geosyst, 2(4): n/a

  • Meng Q, Liu Z, Bruch A A, Liu R, Hu F (2012). Palaeoclimatic evolution during Eocene and its influence on oil shale mineralisation, Fushun basin, China. J Asian Earth Sci, 45: 95–105

    Article  Google Scholar 

  • Nesbitt H W, Young G M (1982). Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 299(5885): 715–717

    Article  Google Scholar 

  • Peters K E, Cassa M R (1994). Applied source rock geochemistry: Chapter 5: Part II. Essential Elements, 93–120

  • Qi H W, Hu R Z, Su W C, Qi L, Feng J Y (2004). Continental hydrothermal sedimentary siliceous rock and genesis of superlarge germanium (Ge) deposit hosted in coal: a study from the Lincang Ge deposit, Yunnan, China. Sci China Ser D Earth Sci, 47(11): 973–984

    Article  Google Scholar 

  • Rimmer S M (2004). Geochemical paleoredox indicators in Devonian-Mississippian black shales, central Appalachian basin (USA). Chem Geol, 206(3–4): 373–391

    Article  Google Scholar 

  • Rimmer S M, Thompson J A, Goodnight S A, Robl T L (2004). Multiple controls on the preservation of organic matter in Devonian-Mississippian marine black shales: geochemical and petrographic evidence. Palaeogeogr Palaeoclimatol Palaeoecol, 215(1–2): 125–154

    Article  Google Scholar 

  • Roser B, Korsch R J T J G (1986). Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio. J Geol, 94(5): 635–650

    Article  Google Scholar 

  • Scotese C R, Song H, Mills B J W, van der Meer D G (2021). Phanerozoic paleotemperatures: the earth’s changing climate during the last 540 million years. Earth Sci Rev, 215: 103503

    Article  Google Scholar 

  • Shi Q, Li C, Wang S, Li D, Wang S, Du F, Qiao J, Cheng Q (2022). Effect of the depositional environment on the formation of tar-rich coal: a case study in the northeastern Ordos Basin, China. J Petrol Sci Eng, 216: 110828

    Article  Google Scholar 

  • Song H, Wang H, Wang F, Guo R, Hu B (2016). Ichnofossils and ichnofabrics in the Lower Permian Taiyuan Formation of North China Basin. Geodin Acta, 28(1–2): 37–52

    Article  Google Scholar 

  • Stock C A, John J G, Rykaczewski R R, Asch R G, Cheung W W L, Dunne J P, Friedland K D, Lam V W Y, Sarmiento J L, Watson R A (2017). Reconciling fisheries catch and ocean productivity. Proc Natl Acad Sci USA, 114(8): E1441–E1449

    Article  Google Scholar 

  • Stüben D, Kramar U, Berner Z, Stinnesbeck W, Keller G, Adatte T (2002). Trace elements, stable isotopes, and clay mineralogy of the Elles II K-T boundary section in Tunisia: indications for sea level fluctuations and primary productivity. Palaeogeogr Palaeoclimatol Palaeoecol, 178(3–4): 321–345

    Article  Google Scholar 

  • Talbot M R (1988). The origins of lacustrine oil source rocks: evidence from the lakes of tropical Africa. Geological Society. 40(6): 29–43

    Article  Google Scholar 

  • Tang D, Shi X, Zhao X, Wang X, Song G (2015). Mo-U Covariation as an important proxy for sedimentary environment redox conditions progress, problems and prospects. Geoscience, 29(1): 1 (in Chinese)

    Google Scholar 

  • Tang X, Zhang J, Wang X, Yu B, Ding W, Xiong J, Yang Y, Wang L, Yang C (2014). Shale characteristics in the southeastern Ordos Basin, China: implications for hydrocarbon accumulation conditions and the potential of continental shales. Int J Coal Geol, 128–129: 32–46

    Article  Google Scholar 

  • Taylor S R, McLennan S M (1985). The Continental Crust: Its Composition and Evolution. Blackwell Scientific Pub

  • Taylor S R, McLennan S M (1995). The geochemical evolution of the continental crust. Rev Geophys, 33(2): 241–265

    Article  Google Scholar 

  • Tenger, Liu W, Xu Y, Chen J (2006). Comprehensive geochemical identification of highly evolved marine carbonate rocks as hydrocarbon-source rocks as exemplified by the Ordos Basin. Sci China Ser D Earth Sci, 49(4): 384–396

    Article  Google Scholar 

  • Tribovillard N, Algeo T J, Lyons T, Riboulleau A (2006). Trace metals as paleoredox and paleoproductivity proxies: an update. Chem Geol, 232(1–2): 12–32

    Article  Google Scholar 

  • Tyson R V (2001). Sedimentation rate, dilution, preservation and total organic carbon: some results of a modelling study. Org Geochem, 32(2): 333–339

    Article  Google Scholar 

  • Wang Q, Jiang F, Ji H, Jiang S, Liu X, Zhao Z, Wu Y, Xiong H, Li Y, Wang Z (2020). Effects of paleosedimentary environment on organic matter enrichment in a saline lacustrine rift basin - A case study of Paleogene source rock in the Dongpu Depression, Bohai Bay Basin. J Petrol Sci Eng, 195: 107658

    Article  Google Scholar 

  • Wedepohl K J P, Earth C (1971). Environmental influences on the chemical composition of shales and clays. Phys Chem Earth, 8: 307–333

    Article  Google Scholar 

  • Wei Z, Wang Y, Wang G, Zhang T, He W, Ma X, Yu X (2020). Enrichment mechanism of the Upper Carboniferous-Lower Permian transitional shale in the east margin of the Ordos Basin, China: evidence from geochemical proxies. Geofluids, 2020: 1–14

    Article  Google Scholar 

  • Wignall P B, Twitchett R J (1996). Oceanic anoxia and the end Permian mass extinction. Science, 272(5265): 1155–1158

    Article  Google Scholar 

  • Wu J, Zhang Y, Zhou H (2020). Groundwater chemistry and groundwater quality index incorporating health risk weighting in Dingbian County, Ordos basin of northwest China. Chem Erde, 80(4): 125607

    Article  Google Scholar 

  • Wu Y, Liu C, Liu Y, Gong H, Awan R S, Li G, Zang Q (2022a). Geochemical characteristics and the organic matter enrichment of the Upper Ordovician Tanjianshan Group, Qaidam Basin, China. J Petrol Sci Eng, 208: 109383

    Article  Google Scholar 

  • Wu Z, He S, He Z, Li X, Zhai G, Huang Z (2022b). Petrographical and geochemical characterization of the Upper Permian Longtan formation and Dalong Formation in the Lower Yangtze region, South China: implications for provenance, paleoclimate, paleoenvironment and organic matter accumulation mechanisms. Mar Pet Geol, 139: 105580

    Article  Google Scholar 

  • Wu Z, Zhao X, Li J, Pu X, Tao X, Shi Z, Sun Y (2021). Paleoenvironmental modes and organic matter enrichment mechanisms of lacustrine shale in the Paleogene Shahejie Formation, Qikou Sag, Bohai Bay Basin. Energy Rep, 7: 9046–9068

    Article  Google Scholar 

  • Xu L, Huang S, Liu Z, Zhang Y, Wen Y, Zhou X, Chen W, Ren Z, Wen J (2022). Paleoenvironment evolutionary characteristics of Niutitang shale in Western Hubei, Middle Yangtze, China. ACS Omega, 7(28): 24365–24383

    Article  Google Scholar 

  • Xu L, Lehmann B, Zhang X, Zheng W, Meng Q (2014). Trace element distribution in black shales from the Kunyang phosphorite deposit and its geological significances. Acta Petrol Sin, 30: 1817–1827

    Google Scholar 

  • Yamamoto K (1987). Geochemical characteristics and depositional environments of cherts and associated rocks in the Franciscan and Shimanto Terranes. Sediment Geol, 52(1–2): 65–108

    Article  Google Scholar 

  • Yang K, Zhang B, Yao Y, Yang H, Zhang H, Xiao W, Wang Y (2022). Organic matter accumulation mechanism and characteristics in marine-continental transitional shale: a case study of the upper Permian Longtan Formation from the Well F5 in Sichuan Basin, China. J Petrol Sci Eng, 208: 109604

    Article  Google Scholar 

  • Yang R, Ma T, Liu W, Fang Y, Xing L (2019). Coupled hydromechanical analysis of gas production in fractured shale reservoir by random fracture network modeling. Int J Appl Mech, 11(3): 1950031

    Article  Google Scholar 

  • Yang X, Yan D, Zhang B, Zhang L, Wei X, Li T, He J, Shangguan Y, Zhang M, She X (2020). The depositional mechanism of organicrich siliceous shales in Upper Yangtze area: response to the Kwangsian Orogeny in south China. J Petrol Sci Eng, 192: 107310

    Article  Google Scholar 

  • Yang Y T, Li W, Ma L (2005). Tectonic and stratigraphic controls of hydrocarbon systems in the Ordos Basin: a multicycle cratonic basin in central China. AAPG Bull, 89(2): 255–269

    Article  Google Scholar 

  • Yu W, Tian J, Wang F, Liang Q, Yang T, Kneller B, Liang X (2022). Sedimentary environment and organic matter enrichment of black mudstones from the upper Triassic Chang-7 member in the Ordos Basin, northern China. J Asian Earth Sci, 224: 105009

    Article  Google Scholar 

  • Zeng S, Wang J, Fu X, Chen W, Feng X, Wang D, Song C, Wang Z (2015). Geochemical characteristics, redox conditions, and organic matter accumulation of marine oil shale from the Changliang Mountain area, northern Tibet, China. Mar Pet Geol, 64: 203–221

    Article  Google Scholar 

  • Zhang K, Li Z, Jiang S, Jiang Z, Wen M, Jia C, Song Y, Liu W, Huang Y, Xie X, Liu T, Wang P, Shan C, Wu Y (2018a). Comparative analysis of the siliceous source and organic matter enrichment mechanism of the Upper Ordovician-Lower Silurian Shale in the Upper-Lower Yangtze Area. Minerals (Basel), 8(7): 283

    Google Scholar 

  • Zhang L, Kou Z, Wang H, Zhao Y, Dejam M, Guo J, Du J (2018b). Performance analysis for a model of a multi-wing hydraulically fractured vertical well in a coalbed methane gas reservoir. J Petrol Sci Eng, 166: 104–120

    Article  Google Scholar 

  • Zhang L, Zhao Q, Peng S, Qiu Z, Feng C, Zhang Q, Wang Y, Dong D, Zhou S (2021). Paleoenvironment and organic matter accumulation mechanism of marine-continental transitional shales: outcrop characterizations of the Carboniferous-Permian strata, Ordos Basin, north China. Energies, 14(21): 7445

    Article  Google Scholar 

  • Zhang P, Yang M, Lu J, Shao L, Wang Z, Hilton J (2022). Low-latitude climate change linked to high-latitude glaciation during the late paleozoic ice age: evidence from terrigenous detrital kaolinite. Front Earth Sci (Lausanne), 10: 956861

    Article  Google Scholar 

  • Zhang W, Yang H, Yang Y, Kong Q, Wu K (2008). Petrology and element geochemistry and development environment of Yanchang Formation Chang-7 high quality source rocks in Ordos Basin. Geochimica, 37(1): 59–64

    Google Scholar 

  • Zhang W, Yang W, Xie L (2017). Controls on organic matter accumulation in the Triassic Chang 7 lacustrine shale of the Ordos Basin, central China. Int J Coal Geol, 183: 38–51

    Article  Google Scholar 

  • Zhao B, Li R, Qin X, Wang N, Zhou W, Khaled A, Zhao D, Zhang Y, Wu X, Liu Q (2021). Geochemical characteristics and mechanism of organic matter accumulation of marine-continental transitional shale of the lower permian Shanxi Formation, southeastern Ordos Basin, north China. J Petrol Sci Eng, 205: 108815

    Article  Google Scholar 

  • Zhou T, Zhou Y, Zhao H, Li M, Mu H (2022). Depositional setting and enrichment mechanism of organic matter of Lower Cretaceous shale in Ri-Qing-Wei Basin in the Central Sulu Orogenic Belt. Front Earth Sci (Lausanne), 9: 808916

    Article  Google Scholar 

Download references

Acknowledgments

This work was supported from the Natural Science Basic Research Program of Shaanxi Province (No. 2020JQ-744), China Postdoctoral Science Foundation (No. 2020M673443), Shaanxi Provincial Education Department general special project (No. 21JK0775) Opening Project of Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Natural Resources (No. KF2021-7) and National Natural Science Foundation of China (Grant No. 4210021463).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Delu Li.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

He, Q., Li, D., Sun, Q. et al. Constraints of palaeoenvironment on organic matter of Benxi Formation shale and discussion on enrichment mechanism under different facies. Front. Earth Sci. (2023). https://doi.org/10.1007/s11707-022-1071-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s11707-022-1071-5

Keywords

Navigation