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| 金衢盆地上震旦统和古生界烃源岩演化程度研究 | |
| 引用本文： | 郑华平,张廷山,王明磊,袁续祖.金衢盆地上震旦统和古生界烃源岩演化程度研究[J].天然气地球科学,2006,17(3):351-354. |
| 作者姓名： | 郑华平 张廷山 王明磊 袁续祖 |
| 作者单位： | 1. 西南石油大学,四川,成都,610500;中国石油浙江油田分公司,浙江,杭州,310013 2. 西南石油大学,四川,成都,610500 3. 西南油气田分公司蜀南气矿,四川,泸州,646000 |
| 基金项目： | 四川省重点学科建设项目 |
| 摘 要： | 金衢盆地的烃源岩主要有2套:一套是盆地基底海相地层,另一套是内陆盆地相地层。其中海相地层中的主力烃源岩层为上震旦统和上古生界石炭―二叠系。以镜质体反射率、热解、牙形刺、孢粉作为划分的主要依据,研究了金衢盆地上震旦统和古生界烃源岩的演化程度。 |
| 关 键 词： | 烃源岩 演化程度 金衢盆地 |
| 文章编号： | 1672-1926（2006）03-0351-04 |
| 收稿时间： | 2006-01-19 |
| 修稿时间： | 2006-04-05 |
EVOLUTIONAL DEGREE OF THE SOURCE ROCK FROM UPPER SINIAN AND THE PALEOZOIC GROUP IN JINQU BASIN |
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| ZHENG Hua-ping,ZHANG Ting-shan,WANG Ming-lei,YUAN Xu-zu.EVOLUTIONAL DEGREE OF THE SOURCE ROCK FROM UPPER SINIAN AND THE PALEOZOIC GROUP IN JINQU BASIN[J].Natural Gas Geoscience,2006,17(3):351-354. | |
| Authors: | ZHENG Hua-ping ZHANG Ting-shan WANG Ming-lei YUAN Xu-zu |
| Affiliation: | 1. Southwest Petroleum University, Chengdu 610500, China ; 2. Zhejiang Exploration Branch, CNPC , Hangzhou 310013, China;3. Shunan Gas Mine of Southwest Oil and Gas Branch, CNPC, Luzhou 646000, China |
| Abstract: | The source rock of Jinqu basin mainly has two set.one set is the stratum of marine facies of the basin base,the other is the stratum of the inland basin. The stratum of main source rock among the marine facies is the upper Sinian and the Paleozoic group. The content of this text is studying evolutive degree of the source rock of the upper Sinian and the Paleozoic group mainly by vitrinite, pyrogenation,conodont and sporopollen. |
| Keywords: | Source rock Evolutive degree Jinqu basin |
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