川西前陆盆地侏罗纪沉积体系发育分布特征及差异性
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摘要
论文以沉积学，层序地层学，地球化学，地震地层学等学科理论为指引，通过对川西前陆盆地侏罗纪野外露头剖面，钻井岩心，测井资料，地球物理资料综合分析，结合镜下普通薄片分析，野外沉积构造分析，砂岩粒度分析，重矿物分析，阴极发光分析，微量元素分析等实验分析，系统的研究了川西前陆盆地侏罗纪地层发育特征，物源特征，沉积体系发育特征，层序地层学特征，阐明了川西前陆盆地侏罗纪各沉积体系发育的差异性特征，主要成果认识如下：
1、通过砂岩阴极发光分析，重矿物分析，微量元素分析，及古水流分析等各种方法和分析手段，针对川西前陆盆地中段重点层位进行了物源分析，认为中侏罗世川西前陆盆地中部沙溪庙期主要有以龙门山北段变质岩为主要母岩和以龙门山中段花岗岩等酸性岩浆岩为主要母岩的2大物源，遂宁期、蓬莱镇期则主要表现为龙门山中段物源，北部地区供给的沉积物较少。
2、根据野外露头、钻井岩芯和测井等资料的综合分析，依据岩石组合、沉积组构、剖面结构和演化序列，提出了侏罗纪川西前陆盆地的沉积体系综合划分方案。识别出冲积扇，河流，三角洲和湖泊4类沉积体系发育类型，总结提出了研究区各主要类型沉积体系的识别划分标志，揭示了曲流河三角洲与辫状河三角洲的时空发育分布特征，建立了沉积模式。其中曲流河三角洲发育于中侏罗统下沙溪庙组和中侏罗统上沙溪庙组沙一段-沙二段；辫状河三角洲发育于下侏罗统自流井组，中侏罗统千佛崖组，中侏罗统上沙溪庙组沙三段-沙四段和上侏罗统遂宁组~蓬莱镇组。
3.通过野外露头与钻井岩心观测，结合测井和地震资料，侏罗纪川西前陆盆地层序界面表现形式有以下5种：不整合面，5大型底冲刷面，间歇暴露面，超覆面，岩性岩相转换面，最大湖泛面；且以此为根据认为侏罗纪川西前陆盆地可以识别出8个三级层序，18个四级层序，系统的研究了各三级级层序发育特征，建立了三级层序地层格架。
4、对盆地层序结构发育进行了类型划分，并进一步研究了盆地内部不同相带短期旋回层序发育特点，总结出了盆地短期旋回的分布规律模式。综合盆地内层序发育的结构特征，可划分出五种层序结构类型，即A型、 B1型、B2型、B3型；和C型。河流-三角洲平原相带内主要的基准面旋回类型以A型为主，少数表现为结构B1；三角洲前缘沉积层序结构类型发育具有多样化，从A到C均有所发育，随着距离岸线越来越远，B3或者C型出现的频率愈来愈多；前三角洲—浅湖主要以B3型和C型旋回结构为主，突出特征是C型越来越发育。
5、对沉积层序充填动力学过程进行了探索性研究，探讨了不同时期、不同相区砂体的结构特征及相互叠置过程。
发生进积作用时，在三角洲平原地区，前一个短期旋回旋回往往被部分侵蚀，基准面旋回叠加式样主要以下降半旋回小于上升半旋回或仅保留了上升期半旋回为主，在三角洲前缘和前三角洲地区，基准面叠加式样表现为下降半旋回大于上升半旋回型或为仅保留了下降半旋回型；当发生加积作用时，基准面相对地表变化不大，整个短期基准面旋回保留相对完全，基准面叠加式样为完全对称型或不完全对称型为主；当处于退积作用阶段时，由于基准面相对地表不断地呈小幅度上升，基准面旋回叠加则主要为保留上升半旋回大于下降半旋回的不完全对称型或仅保留上升半旋回为特点。
6、在沉积体系类型特征和层序地层研究的基础上，系统编制了川西前陆盆地侏罗纪各主要层序的区域岩相古地理图，揭示了整个盆地古地理格局、发育特征及其演化。尤其是针对中侏罗统上沙溪庙组至上侏罗统蓬莱镇组，采用4级层序为编图单元，详细阐述了不同时期各个沉积体系发育分布特征及其差异性。
Guided by sedimentology, sequence stratigraphy, geochemistry, seismic stratigraphy andso on, integrated researhed the outcrops, cores,logging data,seismic data and geochemistrydata during Jurassic in the western Sichuan foreland Basin，combined with thin sandstonesection analysis，sedimentary structure mark analysis，sandstone grain size analysis，heavymineral analysis, cathodoluminescenc analysis, trace elements analysis and so on, thecharacteristics of stratigraphy, provenance, sedimentary system, sequence stratigraphy hadbeen researched, the rugulation and difference of every sedimentary system had been detailedresearched. The main achievements as follow were obtained:
1.According to cathodoluminescenc analysis, heavy mineral analysis, trace elementsanalysis, paleocurrent analysis and so on, founding that during the Shaximiao Stage of MiddleJurassic there were two places provided sediments, which were metamorphic rocks from thenorth part of Longmenshan and acidic rocks from the middle part of Longmenshan. Duringthe Suining and Penglaizhen Stage of Later Jurassic，the sediment mainly came form themiddle part of Longmenshan, rarely came from the north part of Longmenshan.
2.According to the outcrops and cores, logging data and seismic figures, combined withrock association, sedimentary fabric, section structure and evolutionary series,4sedimentarysystem were recognized, alluvial fan sedimentary system, fluvial sedimentary system,deltasedimentary system and lake sedimentary system.The distribution characteristics ofmeandering river delta and braided river delta has been revealed,and the sedimentary modelbuilt. meandering river delta developed during the Lower Shaximiao Stage to menber2ofUpper Shaximiao Stage, other time, braided river delta developed.
3.According to the outcrops and cores,combined with logging data and seismic figures,5typical sequence surfaces were found,which were surface of unconformity, surface of erosion,surface of onlap,transition surface of rock character and facies and flooding transgressivesurface. And then8third-order sequence and18forth-order sequence were recognized,thecharacters of each third-order sequence detailed researched, and third-order sequenceframework had been built.
4.On the basis of sequence texture division, the short-term base-level cycles’characteristics of different facies(sedimentary) studied, and sumed up the distribution characteristics of short-term base-level cycles.There were5short-term base-level cyclestexture, which were type A, type B1, type B2, type B3and type C. Type A mainly developed inthe Fluvial-Delta plain sedimentary system, Type A to type C could be found in the Delatforntier sedimentary system, the developed sequence texture type determined by the distancefar from the coastline, the far from the coastline,the more occurrence of type B3or type C.Prodelta-shallow lake sedimentary system mainly developed type B3and type C, especiallytype C developed frequently.
5. Sequence of sedimentary filling dynamics has been discussed. During the progradationstage, only ascending hemicycles sediments or ascending hemicycles sediments more thandescending hemicycles sediments was the mainly texture of base-level cycles within the Deltaplain, only descending hemicycles sediments or ascending hemicycles sediments less thandescending hemicycles sediments was the mainly texture of base-level cycles within the Deltafrontier and prodelta. During the aggradation stage,bese-level cycly rarely changed, texture ofbase-level cycles fully developed, which types mainly Type B or Type C. During theretrogradation, bese-level cycle sustained tiny rised, the texture of base-level cyclescharacteristics showed, only ascending hemicycles sediments or ascending hemicyclessediments more than descending hemicycles sediments.
6.On the baisi of studying the characteristics of depositional system and sedimentarysequence, the regional sequence-based lithofacies-paleogeographic maps of Jurassic in thewestern Sichuan Foreland basin are compiled by choosing different sequence cycles as theisochronous mapping unit.,
This paper demonstrats in details the characteristics of lithofacies aleogeography and theirevolution during different fourth sequence cycles development from MSQ8to MSC18duringthe Upper Shaximiao Stage of Middle Jurassic to Penglaizheng Stage of Upper Jurassic.The difference and distribution characters of different sediment system during the differentstage was discussed in detail.
1、通过砂岩阴极发光分析，重矿物分析，微量元素分析，及古水流分析等各种方法和分析手段，针对川西前陆盆地中段重点层位进行了物源分析，认为中侏罗世川西前陆盆地中部沙溪庙期主要有以龙门山北段变质岩为主要母岩和以龙门山中段花岗岩等酸性岩浆岩为主要母岩的2大物源，遂宁期、蓬莱镇期则主要表现为龙门山中段物源，北部地区供给的沉积物较少。
2、根据野外露头、钻井岩芯和测井等资料的综合分析，依据岩石组合、沉积组构、剖面结构和演化序列，提出了侏罗纪川西前陆盆地的沉积体系综合划分方案。识别出冲积扇，河流，三角洲和湖泊4类沉积体系发育类型，总结提出了研究区各主要类型沉积体系的识别划分标志，揭示了曲流河三角洲与辫状河三角洲的时空发育分布特征，建立了沉积模式。其中曲流河三角洲发育于中侏罗统下沙溪庙组和中侏罗统上沙溪庙组沙一段-沙二段；辫状河三角洲发育于下侏罗统自流井组，中侏罗统千佛崖组，中侏罗统上沙溪庙组沙三段-沙四段和上侏罗统遂宁组~蓬莱镇组。
3.通过野外露头与钻井岩心观测，结合测井和地震资料，侏罗纪川西前陆盆地层序界面表现形式有以下5种：不整合面，5大型底冲刷面，间歇暴露面，超覆面，岩性岩相转换面，最大湖泛面；且以此为根据认为侏罗纪川西前陆盆地可以识别出8个三级层序，18个四级层序，系统的研究了各三级级层序发育特征，建立了三级层序地层格架。
4、对盆地层序结构发育进行了类型划分，并进一步研究了盆地内部不同相带短期旋回层序发育特点，总结出了盆地短期旋回的分布规律模式。综合盆地内层序发育的结构特征，可划分出五种层序结构类型，即A型、 B1型、B2型、B3型；和C型。河流-三角洲平原相带内主要的基准面旋回类型以A型为主，少数表现为结构B1；三角洲前缘沉积层序结构类型发育具有多样化，从A到C均有所发育，随着距离岸线越来越远，B3或者C型出现的频率愈来愈多；前三角洲—浅湖主要以B3型和C型旋回结构为主，突出特征是C型越来越发育。
5、对沉积层序充填动力学过程进行了探索性研究，探讨了不同时期、不同相区砂体的结构特征及相互叠置过程。
发生进积作用时，在三角洲平原地区，前一个短期旋回旋回往往被部分侵蚀，基准面旋回叠加式样主要以下降半旋回小于上升半旋回或仅保留了上升期半旋回为主，在三角洲前缘和前三角洲地区，基准面叠加式样表现为下降半旋回大于上升半旋回型或为仅保留了下降半旋回型；当发生加积作用时，基准面相对地表变化不大，整个短期基准面旋回保留相对完全，基准面叠加式样为完全对称型或不完全对称型为主；当处于退积作用阶段时，由于基准面相对地表不断地呈小幅度上升，基准面旋回叠加则主要为保留上升半旋回大于下降半旋回的不完全对称型或仅保留上升半旋回为特点。
6、在沉积体系类型特征和层序地层研究的基础上，系统编制了川西前陆盆地侏罗纪各主要层序的区域岩相古地理图，揭示了整个盆地古地理格局、发育特征及其演化。尤其是针对中侏罗统上沙溪庙组至上侏罗统蓬莱镇组，采用4级层序为编图单元，详细阐述了不同时期各个沉积体系发育分布特征及其差异性。
Guided by sedimentology, sequence stratigraphy, geochemistry, seismic stratigraphy andso on, integrated researhed the outcrops, cores,logging data,seismic data and geochemistrydata during Jurassic in the western Sichuan foreland Basin，combined with thin sandstonesection analysis，sedimentary structure mark analysis，sandstone grain size analysis，heavymineral analysis, cathodoluminescenc analysis, trace elements analysis and so on, thecharacteristics of stratigraphy, provenance, sedimentary system, sequence stratigraphy hadbeen researched, the rugulation and difference of every sedimentary system had been detailedresearched. The main achievements as follow were obtained:
1.According to cathodoluminescenc analysis, heavy mineral analysis, trace elementsanalysis, paleocurrent analysis and so on, founding that during the Shaximiao Stage of MiddleJurassic there were two places provided sediments, which were metamorphic rocks from thenorth part of Longmenshan and acidic rocks from the middle part of Longmenshan. Duringthe Suining and Penglaizhen Stage of Later Jurassic，the sediment mainly came form themiddle part of Longmenshan, rarely came from the north part of Longmenshan.
2.According to the outcrops and cores, logging data and seismic figures, combined withrock association, sedimentary fabric, section structure and evolutionary series,4sedimentarysystem were recognized, alluvial fan sedimentary system, fluvial sedimentary system,deltasedimentary system and lake sedimentary system.The distribution characteristics ofmeandering river delta and braided river delta has been revealed,and the sedimentary modelbuilt. meandering river delta developed during the Lower Shaximiao Stage to menber2ofUpper Shaximiao Stage, other time, braided river delta developed.
3.According to the outcrops and cores,combined with logging data and seismic figures,5typical sequence surfaces were found,which were surface of unconformity, surface of erosion,surface of onlap,transition surface of rock character and facies and flooding transgressivesurface. And then8third-order sequence and18forth-order sequence were recognized,thecharacters of each third-order sequence detailed researched, and third-order sequenceframework had been built.
4.On the basis of sequence texture division, the short-term base-level cycles’characteristics of different facies(sedimentary) studied, and sumed up the distribution characteristics of short-term base-level cycles.There were5short-term base-level cyclestexture, which were type A, type B1, type B2, type B3and type C. Type A mainly developed inthe Fluvial-Delta plain sedimentary system, Type A to type C could be found in the Delatforntier sedimentary system, the developed sequence texture type determined by the distancefar from the coastline, the far from the coastline,the more occurrence of type B3or type C.Prodelta-shallow lake sedimentary system mainly developed type B3and type C, especiallytype C developed frequently.
5. Sequence of sedimentary filling dynamics has been discussed. During the progradationstage, only ascending hemicycles sediments or ascending hemicycles sediments more thandescending hemicycles sediments was the mainly texture of base-level cycles within the Deltaplain, only descending hemicycles sediments or ascending hemicycles sediments less thandescending hemicycles sediments was the mainly texture of base-level cycles within the Deltafrontier and prodelta. During the aggradation stage,bese-level cycly rarely changed, texture ofbase-level cycles fully developed, which types mainly Type B or Type C. During theretrogradation, bese-level cycle sustained tiny rised, the texture of base-level cyclescharacteristics showed, only ascending hemicycles sediments or ascending hemicyclessediments more than descending hemicycles sediments.
6.On the baisi of studying the characteristics of depositional system and sedimentarysequence, the regional sequence-based lithofacies-paleogeographic maps of Jurassic in thewestern Sichuan Foreland basin are compiled by choosing different sequence cycles as theisochronous mapping unit.,
This paper demonstrats in details the characteristics of lithofacies aleogeography and theirevolution during different fourth sequence cycles development from MSQ8to MSC18duringthe Upper Shaximiao Stage of Middle Jurassic to Penglaizheng Stage of Upper Jurassic.The difference and distribution characters of different sediment system during the differentstage was discussed in detail.
引文
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