珲春盆地低煤阶煤层气富集规律Low rank enrichment of coalbed methane in Hunchun basin
王有智
WANG Youzhi
摘要(Abstract):
珲春盆地煤层气取得工业突破对我国低煤阶含煤盆地的煤层气勘探具有重要意义。通过对珲春盆地低煤阶煤层气成藏条件的深入剖析,探讨了低煤阶煤层气富集的主控因素及其成藏模式。结果表明,珲春盆地具有煤阶低、煤层多、煤层薄的特点,构造作用、沉积特征和岩浆岩侵入是其富集成藏的主控因素。盆地西部的褶皱和断层伴生带不仅为生物气创造有利环境,而且为煤层气二次成藏提供场所,形成"连续褶皱"富气模式;沼泽和天然堤微相的垂向叠置,使得作为煤层直接顶底板的泥岩和致密砂岩对煤层气起到更好的封闭作用;局部辉绿岩侵入体促使煤层再次生气,同时大大改善了煤岩的物性。因此,珲春盆地西部是煤层气高产富集区,具有巨大勘探开发潜力。
To obtain the industrial breakthrough of coalbed methane in Hunchun basin has great significance for the exploration of coalbed methane(CBM) in China's low rank coal basins. Through the deepened analysis on the reservoir-forming conditions of coalbed methane of low rank coal in Hunchun basin, the paper discussed the major controlling factors of CBM enrichment of low rank coal and its reservoir-forming model. The results show that Hunchun basin is characterized by low coal rank, multiple and thin seams. There are three main control factors for CBM accumulation, including tectonic setting, sedimentary characteristics and magmatic rock intrusion. The area with faults and folds in the west of the basin has not only created the favorable environments for biogas, but also provided the place for secondary reservoir forming, eventually forming the gas enrichment model of "continuous fold". The vertical superimposition of microfacies of marshes and natural levee which made mudstone and dense sandstone as the direct roof and floor of coal seams have better sealing effect for CBM, local diabase intrusion inside coal seams made again hydrocarbon to be generated, and greatly improved the physical properties of coal. Therefore, the west of Hunchun basin is an area rich in CBM and has a great potential for exploration and development.
关键词(KeyWords):
珲春盆地;低煤阶;成藏条件;富集规律
Hunchun basin;low rank coal;reservoir-forming conditions;enrichment law
基金项目(Foundation): 中石油科技攻关项目(2010E-2201;2012E-2603)
作者(Author):
王有智
WANG Youzhi
参考文献(References):
- [1]张建博,王红岩,赵庆波.中国煤层气地质[M].北京:地质出版社,2000:15–30.
- [2]中国煤田地质总局.中国煤层气资源[M].徐州:中国矿业大学出版社,1999:26–87,130–135.
- [3]李巧梅,王瑞英,陈宏亮.低阶煤盆地煤层气勘探的几点思考[J].吐哈油气,2004,9(3):267–272.
- [4]刘洪林.中国煤层气资源评价[R].廊坊:中国石油勘探开发研究院廊坊分院,2006.
- [5]SCOTT A R.KAISER W R,AYERS W B,et al.Thermogenic and secondary biogenic gases,San Juan Basin,Colorado and New Mexico:Implications for coalbed gas producibility[J].AAPG Bulletin,1994,78(8):1186–1209.
- [6]SCOTT A R.Composition and orgin of coalbed gases from selected basin in the United States[C]//Proceedings of the1993 International Coalbed Methane Symposium.Birmingham,Alabama:The University of Alabama/Tuscaloosa,1993:209–222.
- [7]傅小康,霍永忠,胡爱梅,等.美国低煤阶煤层气的勘探开发现状[J].中国煤炭,2006,32(5):75–77.
- [8]王红岩,李景明,李剑,等.中国不同煤阶煤的煤层气成藏特征对比[C]//中国煤炭学会煤层气专业委员会.中国煤层气勘探开发利用技术进展.北京:地质出版社,2006:191–193.
- [9]王勃,李景明,张义,等.中国低煤阶煤层气地质特征[J].石油勘探与开发,2009,36(1):30–33.
- [10]孙平,王勃,孙粉锦,等.中国低煤阶煤层气成藏模式研究[J].石油学报,2009,30(5):648–653.
- [11]李五忠,田文广,孙斌,等.低煤阶煤层气成藏特点与勘探开发技术[J].天然气工业,2008,28(3):23–25.
- [12]孙平,刘洪林,巢海燕,等.低煤阶煤层气勘探思路[J].天然气工业,2008,28(3):19–22.
- [13]赵群,康永尚,王红岩,等.浅层低煤阶煤层气成藏条件分析[J].西安石油大学学报:自然科学版,2006,21(5):20–23.
- [14]李景林,郭逐申,武敬东,等.珲春煤田煤层气开发储层改造工艺应用研究[J].中国煤炭地质,2012,24(11):22–27.
- [15]崔玉环,王生辉,马银起,等.珲春盆地煤层气赋存特征及其开发前景分析[J].煤炭技术,2005,24(6):102–104.
- [16]王青元,杨天鸿,李铁良,等.八连城煤矿19号煤层瓦斯地质规律研究[J].煤炭科学技术,2012,40(1):115–117.
- [17]叶建平,武强,王子和.水文地质条件对煤层气赋存的控制作用[J].煤炭学报,2001,26(5):459–462.
- [18]姚艳斌,刘大锰,黄文辉,等.两淮煤田煤储层孔-裂隙系统与煤层气产出性能研究[J].煤炭学报,2006,31(2):163–168.
- [19]闫宝珍,王延斌,丰庆泰,等.基于地质主控因素的沁水盆地煤层气富集划分[J].煤炭学报,2008,33(10):1102–1106.
- [20]赵庆波,张公明.煤层气评价重要参数及选区原则[J].石油勘探与开发,1999,26(2):23–26.
- [21]陈振宏,贾承造,宋岩,等.构造抬升对高、低煤阶煤层气藏储集层物性的影响[J].石油勘探与开发,2007,34(4):461–464.
- [22]李贵中,王红岩,吴立新,等.煤层气向斜控气论[J].天然气工业,2005,25(1):26–28.
- [23]张慧,郑玉柱,席先武.铁法盆地煤变质作用及煤层气生成特征[J].煤田地质与勘探,1999,27(4):30–33.
- [24]范立明,李世刚,孙震.铁法煤田火成岩规律研究[J].煤炭技术,2004,23(3):107–108.
- [25]刘锦,王宇林.铁法矿区侵入岩特征及侵入机制[J].中国煤炭地质,2009,21(9):29–31.
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