Abstract
There are many structural buried hills in the east of Tazhong Low Rise that have significantly valuable for oil/gas exploration and research. In this work, geochemical and geological methods were used to research the complicated diagenetic process of Yingshan carbonate. The Yingshan carbonate underwent four diagenetic stages with three types of calcite, which diagenetic environment was complex and variable. During the Early Ordovician of syndiagenetic stage, the high-magnesium CI calcite develops along the micro-fracture and has no or very weakly cathodoluminescence color. In the following early diagenetic, the Yingshan carbonate subsided and developed the CIII calcite along the corroded fissure and pressolved sutures. After the M1 buried hill formed during the Late Silurian, the Yingshan carbonate experience the supergene stage, and suffered the weathering and denudation for a long period. During the Carboniferous karst, two cave horizons developed in the M1 buried hill, corresponding with two sets of Carboniferous carbonate rocks by the stratigraphic correlation. The cement CII calcite contains less Sr, Na, Mg, and more Mn and Fe than sea water, showing bright red in the cathodoluminescence. During the following middle and late diagenetic stage, M1 buried hill underwent a process of persistent burial and slight uplifting with CIII calcite cementing from the formation water. During the Permian, the hydrothermal fluid intensely influenced the buried hill, leaving the hydrothermal minerals.
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References
Aguilera R, van Poollen HK (1979) Naturally fractured reservoirs. Part 12. Studies show occurrence of fractured reservoirs. Oil Gas J 77:70–76
Baker PA, Burns SJ (1985) Occurrence and formation of dolomite in organic-rich continental margin sediments. AAPG Bull 69:1917–1930
Bao JP, Kong J, Zhu CS, Zhang QC, Li M, Lu YH, Zhang WY (2012) Geochemical characteristics of a novel kind of marine oils from Tarim Basin. Acta Sedimentol Sin 30(3):580–587
Bencini A, Turi A (1974) Mn distribution in the Mesozoic carbonate rocks from Lima Valley, northern Apennines. J Sediment Res 44(3):774–782
Brand U, Veizer J (1980) Chemical diagenesis of a multicomponent carbonate system-1: trace elements. J Sediment Petrol 50:1219–1236
Bulling TP, Breyer JA (1989) Exploring for subtle traps with high-resolution Paleogeographic maps: Reklaw 1 Interval (Eocene), South Texas. AAPG Bull 73:24–39
Cai Y, Zhang Q, Zhang YB, Li KW (2015) Strontium isotopic geochemistry of hydrothermal calcites in carbonate-hosted talc deposits at Zhenxu in central Guangxi Province, South China. Geochimica 44(5):427–437
Chang H, Gong Q, Ouyang R, Huang JF, Yang XW (2003) The characteristics of igneous rocks and their influences to petroleum exploration in the center of Tarim Basin. Geophys Prospect Pet 42:49–53
Chen DZ (2008) Structure-controlled hydrothermal dolomitization and hydrothermal dolomite reservoirs. Oil Gas Geol 29(5):614–622
Chen ZQ, Shi GR (2003) Late Paleozoic depositional history of the Tarim basin, northwest China: an integration of biostratigraphic and lithostratigraphic constraints. AAPG Bull 87:1323–1354
Chen JS, Li Z, Wang ZY, Tan SC, Li L, Ma Q (2007) Paleokarstification and reservoir distribution of Ordovician carbonates in Tarim Basin. Acta Sedimentol Sin 25:858–868
Cuong T, Warren J (2009) Bach ho field, a fractured granitic basement reservoir, Cuu Long Basin, offshore SE Vietnam: a “buried-hill” play. J Pet Geol 32(2):129–156
Davies GR, Smith LB (2006) Structurally controlled hydrothermal dolomite reservoir facies: an overview. AAPG Bull 90(11):1641–1690
Du YB, Tian NX, Wang PJ, Tu ZM, Cheng QF (2005) Genetic analysis of Ordovician oil and gas trap developed on top of buried carbonate karst hill, Central Tarim Basin, NW China. Glob Geol 24(2):161–167
Fang DJ, Shen ZY (2001) Phanerozoic apparent polar-wander paths of Tarim and plate motion. J Zhejiang Univ (Sci Ed) 28:100–106
Gu JY, Zhou XX, Li M, Li XD, Zhang GY (1999) Hydrocarbon prospecting in Ordovician carbonate buried-hill in Lunnan area, Tarim Basin. Pet Explor 4:23–27
Guo JH, Zeng YF, Zhai YH, Gao ZZ (1996) On the carboniferous sequence stratigraphy in the Tazhong area, Xinjiang—a model of the sequence stratigraphy framework of intracratonic depressional basins. Acta Geol Sin 70:361–373
He H, Peng SP, Shao LY (2004) Trace elements and sedimentary settings of Cambrian-Ordovician carbonates in Bachu area, Tarim Basin. Xinjiang Pet Geol 25:631–633
Hemming NG, Meyers WJ, Grams JC (1989) Cathodoluminescence in diagenetic calcites; the roles of Fe and Mn as deduced from electron probe and spectrophotometric measurements. J Sediment Petrol 59(3):404–411
Hyung H, Kim JH (2006) A mechanistic study on boron rejection by sea water reverse osmosis membranes. J Membr Sci 286:269–278
Jia CZ, Wei GQ, Yao HJ, Li LC (1995) Tectonic evolution and regional structural geology in the Tarim Basin. Petroleum Industry Press, Beijing, pp 42–103
Jiang P (2000) A pool formation analysis for Qianmiqiao buried hill structure. Pet Explor Dev 27:14–16
Jin ZJ (2010) Petroliferous features of marine carbonate strata and hydrocarbon resource prospects in China. Front Sci 1:11–23
Jin ZJ, Zhang LP, Yang L, Hu WX (2002) Primary study of geochemical features of deep fluids and their effectiveness on oil/gas reservoir formation in sedimental Basins. Earth Sci 27:659–665
Keith ML, Weber JN (1964) Carbon and oxygen isotopic composition of selected limestone and fossils. Geochim Cosmochim Acta 28:1787–1816
Koning T, Darmono FX (1984) The geology of the Beruk Northeast field, Central Sumatra: oil production from Pre-Tertiary basement rocks. In: 13th AAPG annual convention proceedings, vol 1, pp 385–406
Lan XD, Liu H, Lü XX, Lan BH (2018) Dolomites of the Yingshan Formation in the Tazhong Low Rise, Tarim Basin: dolomitisation and reformation model. Geosci J 22(1):47–64
Landes KK, Amoruso JJ, Charlesworth LJ, Heany F, Lesperance PJ (1960) Petroleum resources in basement rocks. AAPG Bull 44:1682–1691
Li SY, Jin FQ, Wang DX (1995) Trace element geochemical characteristics of diagenesis of carbonate rocks. Exp Pet Geol 17(1):55–62
Li P, Chen JS, Wang ZY (2006) The controlling factors and types of the Ordovician carbonate reservoir in Tazhong Area. Gas Prospect Exploit 26:37–42
Li BL, Guan SW, Li CX, Wu GH, Yang HJ, Han JF, Luo CS, Miao JJ (2009) Paleo-tectonic evolution and deformation features of the lower Uplift in the Central Tarim Basin. Geol Rev 55:521–530
Liu SP, Guo JH, Gao ZZ (1996) Statistical analysis of trace element data in Lower Carboniferous rocks in Damusi Section, Southwestern Tarim Basin. J Jianghan Pet Inst 18:25–30
Liu W, Zhang XY, Gu JY (2009) Sedimentary environment of Lower-Middle Ordovician Yingshan Formation in Mid-Western Tarim Basin. Acta Sedimentol Sin 27:435–442
Loucks RG (1999) Paleocave carbonate reservoirs: origins, burial-depth modifications, spatial complexity, and reservoir implications. AAPG Bull 83:1795–1834
Lü XX, Jin ZJ (2000) Distribution patterns of oil-gas fields in the carbonate rock. Acta Pet Sin 21:8–12
Lü XX, Yang HJ, Xu SL, Xie QL, Liu LF (2004) Petroleum accumulation associated with volcanic activity in the Tarim Basin: taking Tazhong-47 Oilfield as an example. Pet Sci 1:30–36
Lü XX, Xie QL, Yang N, Li JJ (2007) Hydrocarbon accumulation in deep fluid modified carbonate rock in the Tarim Basin. Chin Sci Bull 52(S1):184–192
Lü XX, Yang N, Zhou XY, Yang HJ, Li JJ (2008) Influence of Ordovician carbonate reservoir beds in Tarim Basin by faulting. Sci China (Ser D) 51:53–60
Ma YS (2000) Chinese marine carbonate oil and gas resource, major scientific and technological problems and countermeasures in exploration. Pet Forum 7:11–14
King RE (1972) Stratigraphic oil and gas fields: classification, exploration methods, and case histories. American Association of Petroleum Geologists Memoir, vol 16, Tulsa, Okla, pp 502–510
Ni SQ, Hou QL, Wang AJ, Ju YW (2010) Geochemical characteristics of carbonate rocks and its geological implications—taking the Lower Palaeozoic carbonate rock of Beijing area as an example. Acta Geol Sin 84(10):1510–1516
P’An CH (1982) Petroleum in basement rocks. AAPG Bull 66(10):1597–1643
Pang XQ (2010) Key challenges and research methods of petroleum exploration in the deep of superimposed basins in western China. Oil Gas Geol 31:517–534
Powers S (1926) Reflected buried hills in the oil fields of Persia, Egypt, and Mexico. AAPG Bull 10:422–442
Qiu NS, Chang J, Zuo YH, Wang JY, Li HL (2012) Thermal evolution and maturation of lower Paleozoic source rocks in the Tarim Basin, northwest China. AAPG Bull 96(5):789–821
Tucker ME, Wright VP (1990) Carbonate sedimentology. Blackwell Scientific Publications, Oxford, pp 314–400
Veizer J, Demovic R (1974) Strontium as a tool in facies analysis. J Sediment Petrol 44(1):93–115
Walters RF (1946) Buried Pre-Cambrian hills in Northeastern Barton County, Central Kansas. AAPG Bull 30:660–710
Wang Y, Ji YL, Xiong JH, Tian HQ (1998) Sequence stratigraphic analysis of the Neodevonian—carboniferous in the Tarim Basin. Acta Geol Sin 16:74–81
Wu GH, Li QM, Zhang BS, Dong LS, Zhang YG, Zhang HQ (2005) Structural characteristics and exploration fields of No.1 Faulted Slope Break in Tazhong area. Acta Pet Sin 26:27–30
Xu GQ, Li GR, Liu SG, Wu HZ, Tian NX, Li ZW (2005) Multiple karst cave horizons in the Early Hercynian weathering crust in the Tarim Basin. Acta Geol Sin 79:557–567
Yang MH (2008) Diversity of buried-hills and comparison of their hydrocarbon—pooling factors in the Bohai Bay Basin. Oil Gas Geol 29:623–633
Yang HJ, Han JF, Sun CH, Wang FH, Zheng Y, Ji YG (2011) A development model and petroleum exploration of karst reservoirs of Ordovician Yingshan Formation in the northern slope of Tazhong palaeouplift. Acta Pet Sin 32:199–205
Yang JF, Zhu WB, Guan D, Zhu BB, Yuan LS, Xiang XM, Su JB, He JW, Wu XH (2016) 3D seismic interpretation of subsurface eruptive centers in a Permian large igneous province, Tazhong Uplift, central Tarim Basin, NW China. Int J Earth Sci 105(8):2311–2326
Yuan XC, Zhao XG, Liu XH, Sun Q, Zhao YF (2001) Formation models of buried hill type pools in Dongpu sag. Pet Explor Dev 28:29–32
Zhang ZS, Han YH (2001) Approach to oil-gas bearing controlling factors of Donghe sandstone traps in Tazhong area of Tarim Basin. Oil Geophys Prospect 36:451–458
Zhang BM, Li XS (2006) The characteristic and evaluation of carbonate reservoir in the Ordovician buried hill of Tazhong area. The internal report in the Tarim oilfield, pp 46–103
Zhang ZS, Li MJ, Liu SP (2002) Generation and evolution of Tazhong low uplift. Pet Explor Dev 29:28–31
Zhao ZJ (2008) Types, accumulation models and exploration concepts of marine carbonate reservoirs. Pet Explor Dev 35:692–703
Zhao ZJ, Zhou XY, Chen XS, Wu XN, Fan GZ (2006) Characteristics of paleokarst reservoirs of Middle-Late Ordovician in Tazhong area, Tarim Basin. Xinjiang Pet Geol 27:660–663
Zhou XY, Wang ZM, Yang HJ, Wang QH, Wu GH (2006) Tazhong Ordovician condensate field in Tarim Basin. Mar Origin Pet Geol 11:45–51
Zhou XY, Li BL, Chen ZX, Yu HF, Jing B (2011) The tectonic genesis and exploration targets of large oil-gas fields in Tazhong area, Tarim Basin. Xinjiang Pet Geol 32:213–217
Zhu DY, Meng QQ (2010) The genesis of silicification in the lower Paleozoic carbonate in the Tarim Basin. Pet Geol Exp 32(4):358–361
Zou CN, Tao SZ (2007) Main controlling factors on the large and medium-sized lithologic and stratigraphic oil/gas fields of marine carbonate rocks. Chin Sci Bull 52:32–39
Acknowledgements
This work was supported by the Fundamental Research Funds for the Central Universities of China (2652018067). The authors would like to thank the researchers in the Tarim Oilfield Company, PetroChina for their helpful discussions and suggestions.
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Lan, X., Liu, H., Lü, X. et al. Geological and geochemical implications of the complicated carbonate diagenetic process in the Lower Ordovician buried hills of the eastern Tazhong Low Rise, NW China, using Well M1 as an example. Carbonates Evaporites 35, 14 (2020). https://doi.org/10.1007/s13146-019-00542-y
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DOI: https://doi.org/10.1007/s13146-019-00542-y