Characteristics and Enrichment Factors of Supergiant Lower Cambrian Longwangmiao Gas Reservoir in Anyue Gas Field: The Oldest and Largest Single Monoblock Gas Reservoir in China

An ultra-deep monoblock marine carbonate gas reservoir with the highest maturity and largest individual scale in China has been discovered in Lower Cambrian Longwangmiao Formation (LF) of Anyue gas field in the last few years. Based on a thorough study on Longwangmiao gas reservoir in the Gaoshiti-Moxi(GM) area, this paper presents the characteristics of such formation in Anyue gas field as follows: ① it is a lithologic-anticlinal gas reservoir developed on a gentle paleo-uplift; ② the gas reservoir is characterized by high temperature and pressure, contains sulfur, and belongs to a dry gas reservoir; and ③ the upper part of the gas reservoir has a good connectivity along with a free of bottom water and edge water, but poor in the lower part, where small scope of enclosed CaCl2 water exists locally. This paper further studies the main control factors for forming this supergiant gas reservoir: ① synsedimentary paleo-uplift controlled the distribution of large-area particle shoal, superimposed by multiple corrosion, which high quality reservoir was formed; ② syngenetic extended aulacogen was filled by mudstone and shale rapidly, resulted in widely distributed thick source rock; ③ synsedimentary gypsum rock and densified carbonate rock formed lateral sealing, multiple type of cap rocks superimposed vertically, therefore excellent closure conditions were formed; ④ large scale of gas reservoir trap was formed at early stage, and it was in a favorable hydrocarbon accumulation pointing area for a long time; and ⑤ the effective time-space matching of numerous hydrocarbon accumulation elements is the key to the formation of the supergiant gas reservoir. The understanding on the formation mechanism and enrichment rule of this ultra-deep, high temperature and high pressure gas reservoir will theoretically enrich the petroleum geology theory, and practically bring important reference to the exploration of large gas fields in the deep ancient craton basins with high maturity and multiple tectonic evolutions in the world.

[1]  P. Zeng,et al.  Enrichment of Shale Gas in Different Strata in Sichuan Basin and its Periphery—The Examples of the Cambrian Qiongzhusi Formation and the Silurian Longmaxi Formation , 2015 .

[2]  Zong-yin Li,et al.  Characteristics and controlling factors of beach-controlled karst reservoirs in Cambrian Longwangmiao Formation, Moxi-Gaoshiti area, Sichuan Basin, NW China , 2014 .

[3]  Wang Xiaobo,et al.  Characteristics of noble gases in the large Gaoshiti-Moxi gas field in Sichuan Basin, SW China , 2014 .

[4]  Hu Wang-shui,et al.  Tectonic evolution of Caledonian Palaeohigh in the Sichuan Basin and its relationship with hydrocarbon accumulation , 2014 .

[5]  C. Zou,et al.  Formation, distribution, resource potential, and discovery of Sinian–Cambrian giant gas field, Sichuan Basin, SW China , 2014 .

[6]  C. Zou,et al.  Theoretical and technical innovations in strategic discovery of a giant gas field in Cambrian Longwangmiao Formation of central Sichuan paleo-uplift, Sichuan Basin , 2014 .

[7]  Dianwei Zhang,et al.  Origin of Marine Sour Natural Gas and Gas-Filling Model in the Puguang Giant Gas Field, Sichuan Basin, China , 2014 .

[8]  Suyun Hu,et al.  Prospect of Ultra-Deep Petroleum Onshore China , 2014 .

[9]  Xiaoqi Wu,et al.  Geochemical Characteristics and Genetic Types of Natural Gas from Tazhong Area in the Tarim Basin, NW China , 2014 .

[10]  C. Zou,et al.  Studies on Gas Origin and Gas Source Correlation Using Stable Carbon Isotopes — A Case Study of the Giant Gas Fields in the Sichuan Basin, China , 2014 .

[11]  Cong Yu,et al.  Genetic Types of the Alkane Gases in Giant Gas Fields with Proven Reserves over 1000×108m3 in China , 2014 .

[12]  Wu Jua Fluid characteristics of Upper Sinian-Lower Cambrian petroliferous strata in Gaoshiti-Moxi structure of Sichuan Basin,China , 2014 .

[13]  Li Yingb Resource potentials of main plays in the petroliferous basins in Russia , 2014 .

[14]  Jiabiao Li,et al.  Carbonate Platforms in the Reed Bank Area, South China Sea: Seismic Characteristics, Development and Controlling Factors , 2013 .

[15]  Zhaoming Wang,et al.  Characteristics and Accumulation Mechanism of Quasi-Layered Ordovician Carbonate Reservoirs in the Tazhong Area, Tarim Basin , 2013 .

[16]  Yue Zhao,et al.  Play Model and Hydrocarbon Transport of Carbonate Reservoirs in Lower Ordovician on Northern Slope of Tazhong Area , 2013 .

[17]  Xiu-yu Li,et al.  Characteristics and Origin of Natural Gases in the Puguang and Maoba Gas Fields, NE Sichuan Basin, China , 2013 .

[18]  Xinyuan Zhou Accumulation Mechanism of Complicated Deep Carbonate Reservoir in the Tazhong Area, Tarim Basin , 2013 .

[19]  Wei Li,et al.  Stratigraphic division and correlation and sedimentary characteristics of the Cambrian in central-southern Sichuan Basin , 2012 .

[20]  Yue Zhao,et al.  Hydrocarbon Distribution Pattern in the Upper Ordovician Carbonate Reservoirs and its Main Controlling Factors in the West Part of Northern Slope of Central Tarim Basin, NW China , 2012 .

[21]  Jin Zhijun,et al.  Phase States of Hydrocarbons in Chinese Marine Carbonate Strata and Controlling Factors for Their Formation , 2012 .

[22]  J. Craig,et al.  From global geology to hydrocarbon exploration: Ediacaran-Early Cambrian petroleum plays of India, Pakistan and Oman , 2012 .

[23]  P. Gao,et al.  Petroleum Systems of the Hebaochang Gas Field in the Southern of Sichuan Basin, SW China , 2012 .

[24]  Hao Xu,et al.  Hydrocarbon-Generation in Cambrian-Silurian High- to Over- Mature Source Rocks, Middle and Upper Yangtze Region, China , 2012 .

[25]  Yue Zhao,et al.  Hydrocarbon Play of Ordovician Carbonate Dominated by Faulting and Karstification—A Case Study of Yingshan Formation on Northern Slope of Tazhong Area in Tarim Basin, NW China , 2011 .

[26]  Yanming Zhu,et al.  Characteristics and Models of Hydrocarbon Accumulation in Eastern Tarim Basin, China , 2011 .

[27]  H. Keyou On Meso-Neoproterozoic primary petroleum resources , 2011 .

[28]  S. Kawahara Erasing fear memories — key receptor and essential timeframe discovered , 2011, Acta Pharmacologica Sinica.

[29]  Hongfeng Yu,et al.  Tracing Hydrocarbons Migration Pathway in Carbonate Rock in Lunnan-Tahe Oilfield , 2010 .

[30]  Hongjie Xu,et al.  Geochemical Evidence for Differential Accumulation of Natural Gas in Shiwu Fault Depression, Songliao Basin, China , 2010 .

[31]  Hongfeng Yu,et al.  Paleozoic Carbonate Hydrocarbon Accumulation Zones in Tazhong Uplift, Tarim Basin, Western China , 2009 .

[32]  Wang Lansheng Geochemical characteristics of bituminous dike in Kuangshanliang area of the Northwestern Sichuan Basin and its significance , 2008 .

[33]  K. Nakayama,et al.  Modelling of Re-Working Carbonate Sediments under Strong Tidal Current Setting , 2001 .

[34]  M. Nemčok,et al.  Sedimentary basins and hydrocarbon habitat at the margin of the Pannonian basin system: introduction , 2001 .

[35]  N. Frewin,et al.  The Dhahaban Petroleum System of Oman , 2000 .

[36]  V. Kuznetsov RIPHEAN HYDROCARBON RESERVOIRS OF THE YURUBCHEN‐TOKHOM ZONE, LENA‐TUNGUSKA PROVINCE, NE RUSSIA , 1997 .