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松辽盆地十屋断陷十屋地区营城组物源体系探讨

         

摘要

在综合分析碎屑颗粒组分、重矿物组合、砂砾岩展布和地层倾角测井等资料的基础上,探讨了十屋断陷十屋地区营城组沉积时期的物源体系特征和分布。碎屑颗粒组分和重矿物分析能指示物源区母岩类型和碎屑物质的搬运方向,砂砾岩展布能指明了碎屑物质的搬运方向和搬运途径,地层倾角测井则指示了古水流的方向。结果表明,十屋地区营城组存在三大物源体系,分别是西北方向以沉积岩和岩浆岩为母岩的西北物源体系、以岩浆岩为母岩的北部斜坡物源体系和以岩浆岩、变质岩为母岩的东部斜坡物源体系,三大物源体系共同控制了十屋地区营城组沉积时期砂体的形成和分布,并且形成了"多物源混源沉积、各物源源间存异、各时期继承发育"的沉积格局。%Several provenances deposition is the result of mixed deposition of detrital materials that came from different provenances and different types of parent rocks.We may neglect the diversity of different provenances if we simply analyse the indexes that can indicate the characteristic of mother rock by calculating the average value.So we should classify the samples which belong to the same provenance at first,then analyze the direction and characteristics of every provenance. This article discussed the provenance system characteristics of Yingcheng Formation in Shiwu fault depression by comprehensive analysis of clastic grain combination,heavy minerals combination,sandy conglomerate distribution,dip logging and other materials.Clastic grain combination can indicate parent rock characteristics of the provenance area,and clastic grain maturation can help to distinguish the transportation direction of fragmentary material.The authors determined three kinds of provenances by classification of the same provenance for clastic grain combination materials of all wells in the study area.The samples of the first kind provenance have the characteristics of " low quartz content,high feldspar and cuttings content,and magmatite is the main cuttings type";the samples of the second kind provenance have the characteristics of " high quartz content,low cuttings content,and magmatite and metamorphic are the main cuttings types";the samples of the third kind provenance have the characteristics of "quartz,feldspar,and cuttings' contents are nealy the same,and sedimentary and magmatite rock are the main cuttings types".Then the three provenance directions above have been determined,and the result are northern provenance,eastern provenance,and northwest provenance respectively. Heavy minerals analysis is also one of the methods of study provenance direction and parent rock characteristics.Three heavy minerals combination areas have been identified by heavy minerals content statistics and combination classification of study area.There are "high zircon content area" in the north,"zircon,garnet,and green shade stone combination area" in the east,and "zircon and garnet combination area" in the westnorth.They stand for the three provenance systems,respectively.These areas indicated that there were three provenance systems exist in Yingcheng Formation of Lishu area. The transport direction and path of detrital material that derived from provenance can be pointed out by analyzing sand bodies distribution characters,and the palaeo-current can be indicated by dipmeter.It were found that there were high content regions of sandy conglomerate in the north,the east and the northwest of the research area,and the direction of sandy conglomerate content declining was the same as the direction of palaeo-current that indicated by dipmeter.The results confirm three provenances which have been identified by analysis all above After analyzing all above,three provenance systems were identified in Shiwu area of Yingcheng Formation.The mother rock in the northwest provenance system are sedimentary rocks and magmatic rocks,mother rock in northern slope provenance is magmatic rocks and mother rock in eastern slope are magmatic rocks and metamorphic rocks.The forming and distribution of sand bodies in Yingcheng Formation of Shiwu area were jointly controlled by the three provenances all above.Consequently,hybrid sedimentation were formed under the control of "multi-provenance,differences existed between each other provenance,and the characteristics of every provenance were inherited between each phase" in Shiwu area.

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