| 塔里木盆地东部地区天然气地球化学特征及成因探讨(之一) |
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| 引用本文： | 陈践发,黄第藩.塔里木盆地东部地区天然气地球化学特征及成因探讨(之一)[J].沉积学报,2000,18(4):606-610. |
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| 作者姓名： | 陈践发 黄第藩 |
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| 作者单位： | 1.中国科学院兰州地质所气体地球化学国家重点实验室,兰州 730000; |
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| 基金项目： | 国家“973”项目,61999043306课题经费支持 |
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| 摘 要： | 塔里木盆地是世界上勘探程度较低的大型盆地之一。近年来在该盆地中进行了大规模的油气勘探,发现了一系列的油、气田,其油、气资源量近似1∶1,说明在该盆地中天然气资源非常丰富。该盆地已发现的天然气主要分布在塔里木盆地东部地区的塔北隆起、塔中隆起和库车拗陷。天然气主要与凝析油及原油伴生。该盆地天然气组分分析表明,已发现的天然气藏绝大多数烃类气体含量大于65%;非烃气体CO2含量小于5%,N2含量小于10%。一些天然气中N2含量达25%到35%。在塔北隆起油气藏中天然气的干湿指数(C1/C2+比值)具有从东到西降低的趋势,天然气中N2含量具有从东到西升高的趋势,天然气甲烷的碳同位素组成也具有由东到西变轻的趋势,结合该区的地质背景可知造成这一趋势的主要因素可能是由于该区下古生界烃源岩热演化程度具有东高西低的特征。
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| 关 键 词： | 塔里木盆地 天然气 碳同位素 |
| 文章编号： | 1000-0550(2000)04-0606-05 |
| 收稿时间： | 1999-07-04 |
| 修稿时间： | 1999年7月4日 |
Geochemical Characteristics and Origin of Natural Gas in the Eastern Tarim Basin(I) |
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| CHEN Jian fa,XU Yong chang,HUANG Di fan.Geochemical Characteristics and Origin of Natural Gas in the Eastern Tarim Basin(I)[J].Acta Sedimentologica Sinica,2000,18(4):606-610. |
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| Authors: | CHEN Jian fa XU Yong chang HUANG Di fan |
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| Institution: | 1.State Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000, P. R. China |
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| Abstract: | Tarim Basin, located in the northwest China, is one of thelargest basins in the world, which has not been well explored. In recent years the large scale of petroleum exploration in the basin has led to the discovery of a series of oil and gas fields, with an approximate 1:1 ratio of oil to gas resource. This means that the natural gas resource is very important for the hydrocarbon resource in the Tarim basin. In this basin most of the discovered gases are condensate-associated gas and oil-associated gas. It is show by chemical components analysis that the content of hydrocarbon of the natural gases from this basin is mostly higher than 65 %. The content of CO2 is mostly less than 5%. The content of N2 is mostly less than 10% and the N2 in some gases reaches 25% to 35%. The Ci/C2+ ratios of gases from Tabei area show a generally decreasing trend from east to west. The content of N2 in gases shows generally Qincreasing trend from east to west. The carbon isotopic composition of methane becomes gradually lighter from east to west. All these may be responsible to the low palaeozoic source rock, of which maturity is generally becoming lower from east to west. |
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| Keywords: | Tarim basin natural gas source rock chemical components carbon isotopic composition |
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