石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2014年
2期
136-143
,共8页
谭先锋%蒋艳霞%田景春%邹国亮%李航%王伟庆
譚先鋒%蔣豔霞%田景春%鄒國亮%李航%王偉慶
담선봉%장염하%전경춘%추국량%리항%왕위경
层序界面%时空属性%孔店组%古近系%济阳坳陷%渤海湾盆地
層序界麵%時空屬性%孔店組%古近繫%濟暘坳陷%渤海灣盆地
층서계면%시공속성%공점조%고근계%제양요함%발해만분지
sequence boundary%spatial and temporal property%Kongdian Formation%Paleogene%Jiyang Depression%Bohai Bay Basin
依据地震、测井、钻井岩心、地球化学等资料,对济阳坳陷古近系孔店组层序界面进行了系统研究。济阳坳陷古近系孔店组层序界面在地震剖面上表现为上超、下超、削蚀、顶超、整一等反射特征;钻井岩心表现为风化壳和岩性岩相转化特征;岩电关系表现为不同类型的岩电突变;地球化学微量元素也表现为突变特征。识别出4个层序界面,分别为一级层序界面TSB1,二级层序界面SSB1,三级层序界面SB1和SB2。 TSB1层序界面主要为区域性质的不整合面,反映了盆地的转化形成;SSB1层序界面主要为构造幕式转化面,反映了盆地断陷作用的阶段变化;SB1和SB2为气候转化面,反映了气候因素引起的旋回变化。层序界面对盆地形成机制、气候变化、幕式断裂活动等具有指示意义。
依據地震、測井、鑽井巖心、地毬化學等資料,對濟暘坳陷古近繫孔店組層序界麵進行瞭繫統研究。濟暘坳陷古近繫孔店組層序界麵在地震剖麵上錶現為上超、下超、削蝕、頂超、整一等反射特徵;鑽井巖心錶現為風化殼和巖性巖相轉化特徵;巖電關繫錶現為不同類型的巖電突變;地毬化學微量元素也錶現為突變特徵。識彆齣4箇層序界麵,分彆為一級層序界麵TSB1,二級層序界麵SSB1,三級層序界麵SB1和SB2。 TSB1層序界麵主要為區域性質的不整閤麵,反映瞭盆地的轉化形成;SSB1層序界麵主要為構造幕式轉化麵,反映瞭盆地斷陷作用的階段變化;SB1和SB2為氣候轉化麵,反映瞭氣候因素引起的鏇迴變化。層序界麵對盆地形成機製、氣候變化、幕式斷裂活動等具有指示意義。
의거지진、측정、찬정암심、지구화학등자료,대제양요함고근계공점조층서계면진행료계통연구。제양요함고근계공점조층서계면재지진부면상표현위상초、하초、삭식、정초、정일등반사특정;찬정암심표현위풍화각화암성암상전화특정;암전관계표현위불동류형적암전돌변;지구화학미량원소야표현위돌변특정。식별출4개층서계면,분별위일급층서계면TSB1,이급층서계면SSB1,삼급층서계면SB1화SB2。 TSB1층서계면주요위구역성질적불정합면,반영료분지적전화형성;SSB1층서계면주요위구조막식전화면,반영료분지단함작용적계단변화;SB1화SB2위기후전화면,반영료기후인소인기적선회변화。층서계면대분지형성궤제、기후변화、막식단렬활동등구유지시의의。
Based on seismic, logging, drilling cores and geochemical data, the sequence boundaries of the Kongdian Formation of Paleogene in the Jiyang Depression were systematically studied. On seismic profiles, the boundaries were featured by onlap, downlap, truncation, toplap and concordance. The drilling cores showed weathering crust and lithology-lithofacies transformation characteristics. The rock-electricity relation indicated different types of mutations. The trace elements also showed mutation characteristics. Four sequence boundaries were identified, including the 1st-order sequence interface TSB1, the 2nd-order sequence interface SSB1 and the 3rd-order sequence interfaces SB1 and SB2. As regional unconformity, the sequence interface TSB1 reflected ba-sin transformation. The sequence interface SSB1 was constructed ceremony conversion surface and showed basin rift stage. The sequence interfaces SB1 and SB2 were climate transformation surfaces and showed the cyclic chan-ges in climate factors. The sequence boundaries were significant for the studies of basin formation, climate change and screen fracture activity.