歧口凹陷中、新生界火成岩储层特征及储层发育控制因素
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摘要
歧口凹陷位于渤海湾盆地黄骅坳陷中北部,是该坳陷中最大的生油凹陷,油气资源丰富,中-新生界火成岩分布广泛。本论文利用岩心观察、普通岩石薄片、铸体薄片、扫描电镜、包裹体测温、压汞实验等分析测试手段,结合盆地埋藏一热演化史模拟和前人烃类充注史等资料,对歧口凹陷中-新生界火成岩的成岩作用和孔隙类型进行了深入的研究,并在此基础上,研究了火成岩储集空间发育的控制因素。研究结果表明,歧口凹陷中、新生界火成岩主要经历了早期和晚期两个成岩作用阶段。早期成岩作用阶段发生的成岩作用类型主要包括：挥发分逸出作用、熔蚀作用、熔结作用、冷凝收缩作用、脱玻化作用、岩浆期后热液沉淀充填作用和岩浆期后热液蚀变作用；晚期成岩作用阶段主要的成岩作用类型包括：机械压实压溶作用、充填作用、胶结作用、交代作用、风化淋滤溶蚀作用和次生溶蚀作用。火成岩在其成岩演化过程中发生了3期溶蚀作用、2期构造作用、2期油气充注作用,以及绿泥石、硅质、碳酸盐等胶结作用。主要的成岩演化序列为：溶蚀作用Ⅰ→构造作用Ⅰ→栉壳状绿泥石→细纤维状绿泥石→硅质Ⅰ→较粗纤维状绿泥石→烃类充注Ⅰ→硅质充填Ⅱ→亮晶方解石Ⅰ→构造作用Ⅱ→溶蚀作用Ⅱ→烃类充注Ⅱ→亮晶方解石Ⅱ→铁方解石(白云石)→硅质充填Ⅲ→溶蚀作用Ⅲ。
歧口凹陷中、新生界火成岩的孔隙类型主要有原生孔隙和次生孔隙两大类。原生孔隙主要包括气孔和残余气孔、火山角砾间孔和原生裂缝,次生孔隙主要包括溶蚀孔(洞、缝)、构造裂缝和风化裂缝。通过大量的孔隙结构参数研究认为,歧口凹陷中新生界辉绿岩的孔喉较大,分选差,连通性较好；玄武岩的孔喉大小中等,分选中等,连通性较差；凝灰岩的孔喉较小,分选性较好,连通性中等。孔隙结构可以分为5种类型,Ⅰ型、Ⅱ型为较好储层,岩性主要为辉绿岩,其次为凝灰岩；Ⅲ型为中等储层,岩性主要为辉绿岩,其次为玄武岩；Ⅳ型为较差储层,岩性主要为玄武岩；Ⅴ型为非储层,岩性主要为凝灰岩。Ⅲ型所占比例最高,达52%,其次是Ⅱ型,Ⅰ型、Ⅳ型、Ⅴ型所占比例较小
歧口凹陷中、新生界火成岩储层发育主要受火成岩岩性和岩相、风化淋滤作用、蚀变作用、火山喷发旋回、构造作用和成岩作用等因素的影响。其中岩性和岩相是储层发育的基础,溶蚀作用是储层发育的决定性因素,构造作用和风化淋滤作用是储层发育的重要条件。
The Qikou depression located in the north-central of Bohai Bay basin is the largest oil generation sag in the Huanghua Depression, rich in oil and gas resources; The volcanic rocks are widely distributed in Mesozoinc Cenozoic. According to a large number of core observations, ordinary microscope, casting thin sections, scanning electron microscope (SEM), fluid inclusion analysis, as well as mercury intrusion experiment data testing, The diagenesision and pore types of volcanic reservoirs in Mesozoic Cenozoic erathem Qikou Depression were in-depth researched.Based on the present research achievement, the controlling factors of the volcanic reservoir space development were puts forward the study focus of this paper, having made the following findings and understanding:
The volcanic rocks of Qikou depression in Mesozoinc Cenozoic erathem have mainly experienced early diagenetic stage and late diagenetic stage. Diagenetic types in early diagenetic stage includes:evolution of volatile component, corrosion effect, sintering effect, condensing contraction, de-vitrification, and post-magmatic hydrothermal precipitates filling and the post-magmatic hydrothermal alteration; Late types in late diagenetic stage includes: mechanical compaction, pressure solution, filling, cementation, metasomatism, weathering-denudated dissolution, and secondary solution effect. According to paleo-temperature, homogenization temperature of fluid inclusions and texture and structure of volcanic rocks, and the authigenic minerals and their occurrence pore types, etc. combined with the history of the basin buried-thermal evolution and hydrocarbon charge filling, research indicates that the volcanic rock diageneses of Qikou depression have undergone three stages of dissolution, two stages of tectonics, two stages of hydrocarbon charging and chlorite cementation, siliceous cementation and carbonate cementation. The main digenetic sequences are dissolution Ⅰ→structure movement Ⅰ→pectinate texture chlorite→fine fibrous chlorite→silicic Ⅰ→coarse fibrous chlorite→hydrocarbon charging→silicic filling Ⅱ→sparry calcite Ⅰ→tectonism Ⅱ→dissolution Ⅱ→hydrocarbon charging Ⅱ→sparry calcite Ⅱ→ferrocalcite→silicic filling Ⅲ→dissolution Ⅲ.
The pore types of volcanic rocks of Qikou depression in Mesozoinc Cenozoic erathem are mainly two categories, primary porosity and secondary porosity. The primary pores include stomata, residual stomata, inter-gravel pores and primary fractures; the secondary pores include:dissolved pores (hole, fractures), structural fractures and weathering fracture. Test results from a great number of records of pore structure parameters have indicated that the diabase in of Qikou depression in Mesozoinc Cenozoic erathem are characterized by good pore throat, poor sorting, better connectivity; the basalt are characterized by medium size pore throat, poor sorting, and poor connectivity; the tuff are characterized by pore throats smaller, sorting good, and medium connectivity. The pore structures are classified into five types. Type Ⅰ,Ⅱ are better reservoirs, whose lithology is mainly diabase and followed by tuff. Type Ⅲ is moderate reservoirs, whose lithology is mainly diabase and followed by basalt. Type Ⅳ is worse reservoir, whose lithology is mainly diabase. Type V is non-reservoir, whose lithology is mainly tuff. Type Ⅲ has the highest proportion, up to52%, and type Ⅱ is the second highest. Type Ⅰ, Ⅳ and Ⅴ have smaller proportion.
The development of volcanic reservoir of Qikou depression in Mesozoinc Cenozoic erathem are mainly affected by the lithology and lithofacies, weathering-leaching, alteration, volcanic eruption cycles, tectonic movement and diagenesis factors. Lithology and lithofacies is the basis of reservoir development; the dissolution is a decisive factor in reservoir development; tectonic movement and weathering-leaching is also an important condition for reservoir development.
歧口凹陷中、新生界火成岩的孔隙类型主要有原生孔隙和次生孔隙两大类。原生孔隙主要包括气孔和残余气孔、火山角砾间孔和原生裂缝,次生孔隙主要包括溶蚀孔(洞、缝)、构造裂缝和风化裂缝。通过大量的孔隙结构参数研究认为,歧口凹陷中新生界辉绿岩的孔喉较大,分选差,连通性较好；玄武岩的孔喉大小中等,分选中等,连通性较差；凝灰岩的孔喉较小,分选性较好,连通性中等。孔隙结构可以分为5种类型,Ⅰ型、Ⅱ型为较好储层,岩性主要为辉绿岩,其次为凝灰岩；Ⅲ型为中等储层,岩性主要为辉绿岩,其次为玄武岩；Ⅳ型为较差储层,岩性主要为玄武岩；Ⅴ型为非储层,岩性主要为凝灰岩。Ⅲ型所占比例最高,达52%,其次是Ⅱ型,Ⅰ型、Ⅳ型、Ⅴ型所占比例较小
歧口凹陷中、新生界火成岩储层发育主要受火成岩岩性和岩相、风化淋滤作用、蚀变作用、火山喷发旋回、构造作用和成岩作用等因素的影响。其中岩性和岩相是储层发育的基础,溶蚀作用是储层发育的决定性因素,构造作用和风化淋滤作用是储层发育的重要条件。
The Qikou depression located in the north-central of Bohai Bay basin is the largest oil generation sag in the Huanghua Depression, rich in oil and gas resources; The volcanic rocks are widely distributed in Mesozoinc Cenozoic. According to a large number of core observations, ordinary microscope, casting thin sections, scanning electron microscope (SEM), fluid inclusion analysis, as well as mercury intrusion experiment data testing, The diagenesision and pore types of volcanic reservoirs in Mesozoic Cenozoic erathem Qikou Depression were in-depth researched.Based on the present research achievement, the controlling factors of the volcanic reservoir space development were puts forward the study focus of this paper, having made the following findings and understanding:
The volcanic rocks of Qikou depression in Mesozoinc Cenozoic erathem have mainly experienced early diagenetic stage and late diagenetic stage. Diagenetic types in early diagenetic stage includes:evolution of volatile component, corrosion effect, sintering effect, condensing contraction, de-vitrification, and post-magmatic hydrothermal precipitates filling and the post-magmatic hydrothermal alteration; Late types in late diagenetic stage includes: mechanical compaction, pressure solution, filling, cementation, metasomatism, weathering-denudated dissolution, and secondary solution effect. According to paleo-temperature, homogenization temperature of fluid inclusions and texture and structure of volcanic rocks, and the authigenic minerals and their occurrence pore types, etc. combined with the history of the basin buried-thermal evolution and hydrocarbon charge filling, research indicates that the volcanic rock diageneses of Qikou depression have undergone three stages of dissolution, two stages of tectonics, two stages of hydrocarbon charging and chlorite cementation, siliceous cementation and carbonate cementation. The main digenetic sequences are dissolution Ⅰ→structure movement Ⅰ→pectinate texture chlorite→fine fibrous chlorite→silicic Ⅰ→coarse fibrous chlorite→hydrocarbon charging→silicic filling Ⅱ→sparry calcite Ⅰ→tectonism Ⅱ→dissolution Ⅱ→hydrocarbon charging Ⅱ→sparry calcite Ⅱ→ferrocalcite→silicic filling Ⅲ→dissolution Ⅲ.
The pore types of volcanic rocks of Qikou depression in Mesozoinc Cenozoic erathem are mainly two categories, primary porosity and secondary porosity. The primary pores include stomata, residual stomata, inter-gravel pores and primary fractures; the secondary pores include:dissolved pores (hole, fractures), structural fractures and weathering fracture. Test results from a great number of records of pore structure parameters have indicated that the diabase in of Qikou depression in Mesozoinc Cenozoic erathem are characterized by good pore throat, poor sorting, better connectivity; the basalt are characterized by medium size pore throat, poor sorting, and poor connectivity; the tuff are characterized by pore throats smaller, sorting good, and medium connectivity. The pore structures are classified into five types. Type Ⅰ,Ⅱ are better reservoirs, whose lithology is mainly diabase and followed by tuff. Type Ⅲ is moderate reservoirs, whose lithology is mainly diabase and followed by basalt. Type Ⅳ is worse reservoir, whose lithology is mainly diabase. Type V is non-reservoir, whose lithology is mainly tuff. Type Ⅲ has the highest proportion, up to52%, and type Ⅱ is the second highest. Type Ⅰ, Ⅳ and Ⅴ have smaller proportion.
The development of volcanic reservoir of Qikou depression in Mesozoinc Cenozoic erathem are mainly affected by the lithology and lithofacies, weathering-leaching, alteration, volcanic eruption cycles, tectonic movement and diagenesis factors. Lithology and lithofacies is the basis of reservoir development; the dissolution is a decisive factor in reservoir development; tectonic movement and weathering-leaching is also an important condition for reservoir development.
引文
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