Reservoir quality and diagenesis of the Permian Lucaogou Formation tight carbonates in Jimsar Sag, Junggar Basin, West China

The Lower Permian Lucaogou Formation in the Jimsar sag, Junggar Basin is a typical tight-oil reservoir in China. For effective exploration and production, the formation of a high-quality reservoir must be thoroughly studied. In this work, the tight-oil reservoir was examined using a variety of methods, including core and thin-section observations, XRD, SEM, CL and fluid inclusion and isotope testing. The tight-oil reservoirs were primarily deposited in saline lake environments, which are dominated by variable admixture of dolomite, quartz, feldspar, tuff, calcite and pyrite. Nine main lithofacies were identified: (1) siliceous mudstone, (2) dolomitic siliceous mudstone, (3) dolomitic mudstone, (4) intraclast packstone/grainstone, (5) ooid grainstone, (6) bioclast grainstone, (7) dolomitic siltstone, (8) mixed siliclastic and intraclast grainstone and (9) brecciated dolomitic mudstone. The pore types are classified into four categories: primary intergranular, moldic, intercrystalline and fracture pores. The properties of tight-oil reservoirs are quite poor, with low porosity (ave. 7.85%) and permeability (ave. 0.110 mD) and a small pore-throat radius (ave. 0.086 μm). The tight-oil reservoirs are dominated by the aggradation of a repetitive meter-scale sedimentary facies succession that records distinct lacustrine expansions and contractions. These tight carbonates have also undergone significant diagenetic alterations, such as dolomitization, dissolution, neomorphism and fracture created intercrystalline and moldic pores, vug and fractures; chemical and mechanical compaction and carbonate cementation have decreased the reservoir quality. Variations in reservoir quality in the Jimusar sag are due to a combination of lithofacies type, high-frequency cyclic depositional architecture, dissolution intensity, dolomitization and tectonic related deformation. This integrated study has helped in understanding the reservoir heterogeneity and hydrocarbon potential of the Jimusar fine-grained rocks.

[1]  H. Qing,et al.  EARLY DOLOMITIZATION AND RECRYSTALLIZATION IN SHALLOW MARINE CARBONATES, MISSISSIPPIAN ALIDA BEDS, WILLISTON BASIN (CANADA): EVIDENCE FROM PETROGRAPHY AND ISOTOPE GEOCHEMISTRY , 2013 .

[2]  P. Homewood The carbonate feedback system; interaction between stratigraphic accomodation, ecological succession and the carbonate factory , 1996 .

[3]  Jean-Marie Rouchy,et al.  Calcitization of Mg–Ca carbonate and Ca sulphate deposits in a continental Tertiary basin (Calatayud Basin, NE Spain) , 2001 .

[4]  M. L. Keith,et al.  Carbon and oxygen isotopic composition of selected limestones and fossils , 1964 .

[5]  Kati Tänavsuu-Milkeviciene,et al.  Evolution of an organic‐rich lake basin – stratigraphy, climate and tectonics: Piceance Creek basin, Eocene Green River Formation , 2012 .

[6]  R. J. Dunham Classification of Carbonate Rocks According to Depositional Textures , 1962 .

[7]  Yongqiang Yang,et al.  Formation of fine crystalline dolomites in lacustrine carbonates of the Eocene Sikou Depression, Bohai Bay Basin, East China , 2016, Petroleum Science.

[8]  Guoqiang Sun,et al.  The origin and formation model of Permian dolostones on the northwestern margin of Junggar Basin, China , 2015 .

[9]  Wang Lan,et al.  Types,characteristics,genesis and prospects of conventional and unconventional hydrocarbon accumulations:taking tight oil and tight gas in China as an instance , 2012 .

[10]  C. Arenas,et al.  Dedolomitization and other early diagenetic processes in Miocene lacustrine deposits, Ebro Basin (Spain) , 1999 .

[11]  R. Swennen,et al.  Calcitization/dedolomitization of Jurassic dolostones (Lebanon): results from petrographic and sequential geochemical analyses , 2008 .

[12]  Zhi Yang,et al.  Concepts, characteristics, potential and technology of unconventional hydrocarbons: On unconventional petroleum geology , 2013 .

[13]  H. Burton Factors Governing Cathodoluminescence in Calcite and Dolomite, and their Implications for Studies of Carbonate Diagenesis , 1991 .

[14]  P. Swart,et al.  The Origin of Dolomites in Tertiary Sediments from the Margin of Great Bahama Bank , 2000 .

[15]  Zhu Xiaomin,et al.  Genetic Mechanism of Dolomitization in Fengcheng Formation in the Wu‐Xia area of Junggar Basin, China , 2012 .

[16]  Zhao-peng Yang,et al.  Characteristics and origin of tuff-type tight oil in Jimusaer sag, Junggar Basin, NW China , 2015 .

[17]  J. Dickson Carbonate identification and genesis as revealed by staining , 1966 .

[18]  K. Raun,et al.  Laboratory animals as surrogate models of human obesity , 2012, Acta Pharmacologica Sinica.

[19]  C. Zou,et al.  Lithofacies and organic geochemistry of the Middle Permian Lucaogou Formation in the Jimusar Sag of the Junggar Basin, NW China , 2016 .

[20]  Andrew S. Cohen,et al.  Paleolimnology: The History and Evolution of Lake Systems , 2004 .

[21]  A. Poszytek,et al.  A tight-gas reservoir in the basinal facies of the Upper Permian Ca1 in the southwestern Zechstein Basin, Poland , 2015, Facies.

[22]  S. Moallemi,et al.  CONTROLS ON RESERVOIR QUALITY IN THE LOWER TRIASSIC KANGAN FORMATION, SOUTHERN PERSIAN GULF , 2008 .

[23]  Kuang Lichu Research of the Tight Oil Reservoir in the Lucaogou Formation in Jimusar Sag: Analysis of Lithology and Porosity Characteristics , 2013 .

[24]  Yong Tang,et al.  Formation conditions and exploration potential of tight oil in the Permian saline lacustrine dolomitic rock, Junggar Basin, NW China , 2012 .

[25]  E. Hiatt,et al.  Shallow‐burial dolomite cement: a major component of many ancient sucrosic dolomites , 2008 .