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南盘江盆地秧1井天然气地球化学特征及成因分析
引用本文:张淑品,赵孟军,张水昌,赵陵,刘培初. 南盘江盆地秧1井天然气地球化学特征及成因分析[J]. 天然气地球科学, 2005, 16(6): 797-803. DOI: 10.11764/j.issn.1672-1926.2005.06.797
作者姓名:张淑品  赵孟军  张水昌  赵陵  刘培初
作者单位:1.中国地质大学能源系,北京 100083;2.中国石油勘探开发研究院,北京 100083;3.中石化南方勘探开发公司研究院贵州科研所,贵州 贵阳,550000
摘    要:
经测试,南盘江盆地秧1井天然气可分为2类:一类为高含N2天然气,N2含量为54.92%~73.89%;另一类为高含CO2天然气,CO2含量大于96%。认为高N2天然气是秧1井乃至南盘江地区具有地质意义的天然气。指出该类天然气甲烷含量一般小于2.5%,几乎不含大于乙烷的烃类组分,CO2含量2.2 7%~9.5 4%;1δ3C1值为-3 3.1 9‰~-3 3.9‰,CO2的1δ3C值为-2 9.3‰~-30.93‰。认为该类天然气不是原油裂解气,也不是源自上二叠统龙潭组的煤成气,而主要是源自中泥盆统泥质烃源岩的干酪根裂解气;中泥盆统泥质烃源岩的“晚期阶段聚气”是造成该地区天然气高含N2、烃类组分碳同位素偏重的主要原因。

关 键 词:天然气组分   天然气同位素   天然气成因   南盘江盆地  
文章编号:1672-1926(2005)06-0797-07
收稿时间:2005-11-03
修稿时间:2005-11-032005-11-11

THE GENESIS AND GEOCHEMICAL CHARACTERISTICS OF NATURAL GAS IN WELL YANG-1 IN NANPANJIANG BASIN
ZHANG Shu-pin,ZHAO Meng-jun,ZHANG Shui-chang,ZHAO Ling,LIU Pei-chu. THE GENESIS AND GEOCHEMICAL CHARACTERISTICS OF NATURAL GAS IN WELL YANG-1 IN NANPANJIANG BASIN[J]. Natural Gas Geoscience, 2005, 16(6): 797-803. DOI: 10.11764/j.issn.1672-1926.2005.06.797
Authors:ZHANG Shu-pin  ZHAO Meng-jun  ZHANG Shui-chang  ZHAO Ling  LIU Pei-chu
Affiliation:1. School of Energy Resources, China University of Geoscience, Beijing 100083, China;2. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 10083, China;3. Guizhou Research Department of Institute, Southern Petroleum Exploration and Development Corp., SINOPEC, Guiyang 550000,China
Abstract:
The gases can mainly be divided into two groups being with high N_2 and high CO_2 in the gas shows of Well Yang1.But,according to the gas analysis and the fact that all gases shows in Nanpangjiang area are with high N_2,the high N_2 gas in Well Yang1 is actual geological significant.The kind of the gas is featured with high N_2 content and heavier isotopic values,the N_2 content is from 54.92% to 73.89%,the δ~(13)C_1 values are from-33.19‰ to-33.9‰.The gas in Well Yang1,not being the cracked gas from crude ...
Keywords:Gas component   Gas isotope  Gas genesis   Nanpangjiang basin.
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