新疆大学地质勘查与工程学院
纸质出版:2010
移动端阅览
[1]田继军.江陵凹陷新沟咀组下段砂岩次生孔隙成因及有利次生孔隙分布区预测[J].新疆大学学报(自然科学版),2010,27(03):368-372.
田继军. 江陵凹陷新沟咀组下段砂岩次生孔隙成因及有利次生孔隙分布区预测[J]. Journal of Xinjiang University (Natural Science Edition in Chinese and English), 2010, 27(3): 368-372.
中—深部砂岩储集空间主要是次生孔隙
其在纵横向上的分布具有非均质性
有机质热演化过程中产生的有机酸对次生孔隙的分布有重要的控制和影响.该文通过对铸体薄片、扫描电镜、阴极发光、物性、碳酸盐含量等多方面资料研究
探讨了次生孔隙带的发育规律
并对该区有利次生孔隙发育区进行了预测
得出荆州背斜带与南部生油洼陷之间的过渡带为次生孔隙最有利发育区
为储层评价提供了有利依据.
The reservoir space of Medium-deep portion sandstone is mainly secondary pores.Its distribution is heterogeneity in vertically and horizontally.The humic acids which come into being at the mature stage of organic matter control and influence secondary pores distribution.In this paper
the data of microscope
the scanning electronic analysis
cathodoluminescence
petrophysical property and carbonate content are presented
the favorable secondary pores-developed area is predicted.The favorable pores-developed area is located at the intermediate belt between Jingzhou anticlinal belt and south generative sag.The research provides evidence for the evaluation of reservoir.
郑浚茂,庞敏.碎屑储集岩的成岩作用研究[M].武汉:中国地质大学出版社,1989.
杨香华,叶加仁,周士科,等.成岩动力学分析与深部储层孔隙预测[J].现代地质,1998,12(1):108-114.
孙永传,李忠,李蕙生,等.中国东部含油气断陷盆地的成岩作用[M].北京:科学出版社,1996.
Giles M R,Boer R B.Secondary porosity,creation of enhanced porosities in the subsurface from the dissolution of caronate cements as a result of cooling formation waters[J].Marine and petroleum Geology,1989,6:261-269.
陈振林,王果寿.松南白垩系次生孔隙演化[J].江汉石油学院学报,1996,18(1):14-18.
Surdam R C,Steven and Laura J.Role of organic and inorganic reactions in development of secondary potosity in sand-stone[J].AAPG Bulletin,1982,66:635-642.
Surdam R C,Crossey L J,Hagen E S,et al.Organic-in-organic intonation and sandstone digenesis[J].AAPG Bulletin,1989,73:1-23.
Stoessell R K,E D Pittman.Secondary porosity revited:the chemistry of dissolution by carboxylic acids and anions[J].AAPG Bulletin,1990,1795-1805.
史基安,晋慧娟,薛莲花.毛明陆等长石砂岩中长石溶解作用发育机理及其影响因素分析[J].沉积学报,1994,12(3):67-75.
0
浏览量
207
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621
