临南洼陷沙河街组油气充注对储层成岩演化及次生孔隙发育的影响
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摘要
论文以临南洼陷为研究区,分析该区沙河街组储层主要的成岩作用包括压实作用、胶结作用、溶蚀作用、交代作用及几种粘土矿物的转化等。经过对本区大量薄片资料分析发现该区沙河街组储层中次生孔隙占主要地位,其主要原因是长石、碳酸盐矿物等的溶蚀。根据本区的具体情况并结合孔隙演化过程及前人的成果对该区的成岩作用阶段进行了划分。
分析了石英、长石、碳酸盐矿物和粘土矿物成岩演化的地球化学过程,并通过研究发现油气注入可能引起储层成岩作用环境的变化。通过对不同含油级别下各种成岩作用演化过程的研究,认为油气充注对储层成岩作用演化在三个方面影响：对储层压实作用的缓冲；抑制石英和伊利石的胶结作用；改造深部溶蚀作用。
根据大量盐水包裹体的均一温度并结合本区的构造发展史,认为该区内油气的充注期次与其构造位置有关,洼陷中心部位油气充注主要有两期即东营期和馆陶期到明化镇期,边缘油气藏只经历一期充注即馆陶期到明化镇期,不同构造位置的油气藏的主要成藏期均为中新世馆陶期至上新世明化镇期。根据冰点温度计算得流体的盐度,经分析发现随含油级别增加盐度略有下降,进一步证实油气充注对成岩作用的影响。
通过定量研究区内含油饱和度与孔隙度的关系,得出以下结论：(1)次生孔隙度与含油级别之间,当含油级别低于或等于油浸时,次生孔隙度随含油级别增加而增加；从油浸到富含油级别时次生孔隙度略有降低。(2)总孔隙度与含油级别大体呈正相关,总孔隙度随着含油级别的增加而增加。
Linnan Subsag is chose to be the research area in the paper. It is analyzed that the main diagenesis of Es reservoirs concludes compaction, cementation, dissolution, metasomatism and conversion of several clay minerals. Based on analysis of numbers of thin section, it is indicated that the secondary pore is dominant in Es reservoirs of this area. The main cause of secondary pore is dissolution of feldspar and carbonate minerals. The diagenesis stages are diparted according to the specific situation of this area and pore-evolution process and the previous results.
Geochemical progress of diagenesis evolution of quartz, feldspar, carbonate minerals and clay minerals is analyzed. It is indicated that the diagenesis environment may be changed as the hydrocarbon filling. According to the research of diagenesis evolution under different oil bearing grade, it is-suggested that hydrocarbon emplacement affects the diagenesis evolution in three areas:cushion the compaction of reservoirs, inhibition of quartz and illite cementation, transformation deep dissolution.
Based on the homogenization temperature of a large number of saline inclusions and structural history, it is considered that charging time related to the structural position:in the center of the subsag there are two periods which is Dongying and Guantao-Minghuazhen Period, and at the edge of the subsag there is only Guantao-Minghuazhen Period. The latter is the main period in both structural positions. The fluid salinity can be calculated using the ice point temperature, which fall a little as the oil bearing grade increases, and this further confirmed the influence of hydrocarbon emplacement to diagenesis.
Quantitative research between oil saturation and porosity gets the conclusion that:(1) between secondary porosity and oil bearing grade, the secondary porosity increases when the oil bearing grade increasing as oil bearing grade under or equal to immersion, little decreases when oil bearing grade reach oil-rich. (2) The total porosity is generally positive correlated with oil bearing grade, which increases as the oil bearing grade increased.
分析了石英、长石、碳酸盐矿物和粘土矿物成岩演化的地球化学过程,并通过研究发现油气注入可能引起储层成岩作用环境的变化。通过对不同含油级别下各种成岩作用演化过程的研究,认为油气充注对储层成岩作用演化在三个方面影响：对储层压实作用的缓冲；抑制石英和伊利石的胶结作用；改造深部溶蚀作用。
根据大量盐水包裹体的均一温度并结合本区的构造发展史,认为该区内油气的充注期次与其构造位置有关,洼陷中心部位油气充注主要有两期即东营期和馆陶期到明化镇期,边缘油气藏只经历一期充注即馆陶期到明化镇期,不同构造位置的油气藏的主要成藏期均为中新世馆陶期至上新世明化镇期。根据冰点温度计算得流体的盐度,经分析发现随含油级别增加盐度略有下降,进一步证实油气充注对成岩作用的影响。
通过定量研究区内含油饱和度与孔隙度的关系,得出以下结论：(1)次生孔隙度与含油级别之间,当含油级别低于或等于油浸时,次生孔隙度随含油级别增加而增加；从油浸到富含油级别时次生孔隙度略有降低。(2)总孔隙度与含油级别大体呈正相关,总孔隙度随着含油级别的增加而增加。
Linnan Subsag is chose to be the research area in the paper. It is analyzed that the main diagenesis of Es reservoirs concludes compaction, cementation, dissolution, metasomatism and conversion of several clay minerals. Based on analysis of numbers of thin section, it is indicated that the secondary pore is dominant in Es reservoirs of this area. The main cause of secondary pore is dissolution of feldspar and carbonate minerals. The diagenesis stages are diparted according to the specific situation of this area and pore-evolution process and the previous results.
Geochemical progress of diagenesis evolution of quartz, feldspar, carbonate minerals and clay minerals is analyzed. It is indicated that the diagenesis environment may be changed as the hydrocarbon filling. According to the research of diagenesis evolution under different oil bearing grade, it is-suggested that hydrocarbon emplacement affects the diagenesis evolution in three areas:cushion the compaction of reservoirs, inhibition of quartz and illite cementation, transformation deep dissolution.
Based on the homogenization temperature of a large number of saline inclusions and structural history, it is considered that charging time related to the structural position:in the center of the subsag there are two periods which is Dongying and Guantao-Minghuazhen Period, and at the edge of the subsag there is only Guantao-Minghuazhen Period. The latter is the main period in both structural positions. The fluid salinity can be calculated using the ice point temperature, which fall a little as the oil bearing grade increases, and this further confirmed the influence of hydrocarbon emplacement to diagenesis.
Quantitative research between oil saturation and porosity gets the conclusion that:(1) between secondary porosity and oil bearing grade, the secondary porosity increases when the oil bearing grade increasing as oil bearing grade under or equal to immersion, little decreases when oil bearing grade reach oil-rich. (2) The total porosity is generally positive correlated with oil bearing grade, which increases as the oil bearing grade increased.
引文
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2.朱筱敏.济阳拗陷古近系碎屑岩储层特征和评价[M].北京：科学出版社,2008,126-144,176-190
3.张金亮,常象春.石油地质学[M].北京：石油工业出版社,2004,84-86
4.张枝焕,王铁冠,常象春.油、水、干层的地球化学识别[J],地质论评,2001,47(5)：516-518
5.胡海燕.油气充注对成岩作用的影响[J],海相油气地,2004,9(1-2)：85-89
6.蔡进功,张枝焕,朱筱敏等.东营凹陷烃类充注与储集层化学成岩作用[J],石油勘探与开发,2003,30(3)：79-83
7.许小琼,张学平.惠民凹陷江家店地区沙三下亚段储集层评价[J],录井工程,2005,16(3)：60-63,68
8刘林玉,陈刚,柳益群等.碎屑岩储集层溶蚀型次生孔隙发育的影响因素分析[J],沉积学报,1998,16(2)：97-99
9.张小莉,查明,杨懿.惠民凹陷沙河街组三段岩性油藏储层孔隙结构特征及油气意义[J],石油与天然气地质,2007,28(2)：287-288 290-291
10.李家强.临南洼陷深层碎屑岩次生孔隙特征及其地质意义[J],断块油气田,2008,15(6)：1-4
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