Lithology identification and lithofacies distribution of Cenozoic volcanic rocks in Wichian Buri Sub-basin of Phetchabun Basin, Thailand
ZHU Xiaoer1, YANG Shangfeng1, SHI Chaoqun2
1. College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China; 2. Exploration and Development Research Institute, Tarim Oilfield Branch Company, CNPC, Korla 841000, China
Abstract:The Cenozoic volcanic rocks are the main hydrocarbon-bearing layers in Wichian Buri Sub-basin of Phetchabun Basin in Thailand. However, the difficulties of lithology identification and uncertainty of lithofacies distribution have seriously restricted further exploration and development of hydrocarbon, due to various rock types related to the complex eruption environments and frequent eruption stages. In this paper, based on the data of cores, rock slice, logging and seismic, the characteristics of volcanic rocks in the study area were studied, and a set of methods for identifying volcanic rocks was established. Meanwhile, the volcanic eruption periods and lithofacies distribution were predicted. The research results show that: (1) weakly alkalic basalts are the main type in the multi-type volcanic rocks, ranging from basic to acid volcanic rocks and lava to pyroclastic in the study area; (2) GR, DEN and Pe well loggings are sensitive to the variation of volcanic rock composition, and FMI can provide information of textures and structures of volcanic rocks, so the combination of the two methods can effectively identify lithology of volcanic rocks; (3) Cenozoic volcanic rocks are the results of three-stage volcanic eruption, and several volcanic lithofacies, such as volcanic vent facies, effusive facies, explosive facies and volcanogenic sedimentary facies, and their distribution was identified and predicted. The conclusions in this paper can provide an effective method for lithology identification of Cenozoic volcanic rocks in study area, and make clear of its lithofacies distribution, which have a certain significance for further exploration and development of hydrocarbon in this area.
[1] 赵文智,邹才能,冯志强,等.松辽盆地深层火山岩气藏地质特征及评价技术[J].石油勘探与开发,2008,35(2):129-142. [2] 王洛,李江海,师永民,等.准噶尔盆地滴西地区石炭系火山岩识别与预测[J].岩石学报,2010,26(1):242-254. [3] 张子枢,吴邦辉.国内外火山岩油气藏研究现状及勘探技术调研[J].天然气勘探与开发,1994,16(1):1-26. [4] Schutter S R.Occurrences of hydrocarbons in and around igneous rocks[J].Geol Soc,London,Spec Publ,2003,214(1):35-68. [5] Sruoga P,Rubinstein N.Processes controlling porosity and permeability in volcanic reservoirs from the Austral and Neuquén basins,Argentina[J].AAPG Bull,2007,91(1):115-129. [6] Feng Z Q.Volcanic rocks as prolific gas reservoir:a case study from the Qingshen gas field in the Songliao Basin,NE China[J].Mar Petrol Geol,2008,25(4/5):416-432. [7] 冯志强,金成志,梁江平,等.大庆油田勘探技术现状及发展方向[J].中国工程科学,2010,12(5):58-62. [8] Zhao W Z,Zou C N,Li J Z,et al.Comparative study on volcanic hydrocarbon accumulations in western and eastern China and its significance[J].Petrol Explor Dev,2009,36(1):1-11. [9] 陈萍,张玲,王惠民.准噶尔盆地油气储量增长趋势与潜力分析[J].石油实验地质,2015,37(1):124-128. [10] 魏国齐,杨威,李剑,等.中国陆上天然气地质特征与勘探领域[J].天然气地球科学,2014,25(7):957-969. [11] 郝家栩,邹立志,陈刚,等.滇西施甸地区卧牛寺组火山岩的地质时代及喷发环境[J].中国地质调查,2015,2(7):40-44. [12] 张照伟,李文渊,张江伟,等.新疆北部晚古生代大规模岩浆作用与成矿耦合关系研究主要进展及成果[J].中国地质调查,2015,2(6):20-25. [13] McCabe R,Celaya M,Cole J,et al.Extension tectonics:the Neogene opening of the north-south trending basins of Central Thailand[J].J Geophys Res,1988,93(B10):11889-11910. [14] Morley C K.Combined escape tectonics and subduction rollback-back arc extension: a model for the evolution of Tertiary rift basins in Thailand,Malaysia and Laos[J].J Geolog Soc,2001,158(3):461-474. [15] Morley C K,Charusiri P,Watkinson I.Structural geology of Thailand during the Cenozoic[M]//Ridd M F,Barber A J,Crow M J.The Geology of Thailand.London:Geological Society,London,2011:273-334. [16] Remus D,Webster M,Keawkan K.Rift architecture and sedimentology of the Phetchabun Intermontane Basin,central Thailand[J].J Southeast Asian Earth Sci,1993,8(1/2/3/4):421-432. [17] Barr S M,Cooper M A.Late Cenozoic basalt and gabbro in the subsurface in the Phetchabun Basin,Thailand:Implications for the Southeast Asian Volcanic Province[J].J Asian Earth Sci,2013,76:169-184. [18] 王德波. 泰国A工区火山岩储层地震预测及展布规律[J].石化技术,2017,24(9):92. [19] Streckeisen A.Classification and nomenclature of volcanic rocks,lamprophyres,carbonatites,and melilitic rocks:recommendations and suggestions of the IUGS Subcommission on the Systematics of Igneous Rocks[J].Geology,1979,7(7):331-335. [20] 邱家骧. 国际地科联火成岩分类学分委会推荐的火山岩分类简介[J].现代地质,1991,5(4):457-468. [21] 杨学峰,李红娟.徐家围子地区火山岩岩相识别机理与方法[J].测井技术,2017,41(6):658-664. [22] 张丽华,张国斌,齐艳萍,等.准噶尔盆地西泉地区石炭系火山岩岩性测井识别[J].新疆石油地质,2017,38(4):427-431. [23] 梁月霞,宋世骏,黄德顺.测井技术识别火山岩储层岩性特征综述[J].国外测井技术,2017,38(4):20-23. [24] 洪有密. 测井原理与综合解释[M].东营:石油大学出版社,1993:229-231. [25] 张莹. 火山岩岩性识别和储层评价的理论与技术研究[D].长春:吉林大学,2010:23-24. [26] 王璞珺,迟元林,刘万洙,等.松辽盆地火山岩相:类型、特征和储层意义[J].吉林大学学报:地球科学版,2003,33(4):449-456. [27] 张姣,辛朝坤,张军勇.火山喷发机构、期次及其控藏作用——以松辽盆地北部莺山凹陷营一段为例[J].石油与天然气地质,2018,39(2):291-299.