华南地质与矿产
華南地質與礦產
화남지질여광산
GEOLOGY AND MINERAL RESOURCES OF SOUTH CHINA
2012年
3期
248-258
,共11页
冯镜权%李勇%段润梅%袁淑琴%肖敦清%丘东洲%彭海燕%韩冰%兰亚萍%庞河清
馮鏡權%李勇%段潤梅%袁淑琴%肖敦清%丘東洲%彭海燕%韓冰%蘭亞萍%龐河清
풍경권%리용%단윤매%원숙금%초돈청%구동주%팽해연%한빙%란아평%방하청
孔店组一段%物源体系%重矿物特征%孔南地区%黄骅坳陷
孔店組一段%物源體繫%重礦物特徵%孔南地區%黃驊坳陷
공점조일단%물원체계%중광물특정%공남지구%황화요함
the first member of Kongdian Formation%provenances system%heavy mineral characteristic%southern Kongdian region%Huanghua Depression
黄骅坳陷孔南地区孔一段砂岩储集物性好,是研究区内重要的含油气层段。根据砂岩成分、重矿物特征、砂体分布体系和地震剖面等资料,对孔店南部孔一段物源方向及物源区母岩性质进行了系统研究。结果表明,孔南地区孔一段物源主要来自于盆地北部、东部、西部和南部,其中北部物源影响范围大,可进一步分出北西和北东两个方向。古物源与成因砂体的空间展布配置关系良好。砂岩组分的Dickinson三角图解显示,物源区构造背景为大陆块区、火山弧区和构造混合区。这些结果反映了黄骅坳陷孔店期盆地在中、新生代构造转型过程中陆内裂陷盆地内形成的具有多物源供给、三分性明显的沉积特点。
黃驊坳陷孔南地區孔一段砂巖儲集物性好,是研究區內重要的含油氣層段。根據砂巖成分、重礦物特徵、砂體分佈體繫和地震剖麵等資料,對孔店南部孔一段物源方嚮及物源區母巖性質進行瞭繫統研究。結果錶明,孔南地區孔一段物源主要來自于盆地北部、東部、西部和南部,其中北部物源影響範圍大,可進一步分齣北西和北東兩箇方嚮。古物源與成因砂體的空間展佈配置關繫良好。砂巖組分的Dickinson三角圖解顯示,物源區構造揹景為大陸塊區、火山弧區和構造混閤區。這些結果反映瞭黃驊坳陷孔店期盆地在中、新生代構造轉型過程中陸內裂陷盆地內形成的具有多物源供給、三分性明顯的沉積特點。
황화요함공남지구공일단사암저집물성호,시연구구내중요적함유기층단。근거사암성분、중광물특정、사체분포체계화지진부면등자료,대공점남부공일단물원방향급물원구모암성질진행료계통연구。결과표명,공남지구공일단물원주요래자우분지북부、동부、서부화남부,기중북부물원영향범위대,가진일보분출북서화북동량개방향。고물원여성인사체적공간전포배치관계량호。사암조분적Dickinson삼각도해현시,물원구구조배경위대륙괴구、화산호구화구조혼합구。저사결과반영료황화요함공점기분지재중、신생대구조전형과정중륙내렬함분지내형성적구유다물원공급、삼분성명현적침적특점。
In the southern Kongdian region of Huanghua Depression, the first member of Kongdian Formation, with fine accumulation properties, is the important exploration intervals in the research area. The authors did a systematic research on the provenance and the characteristics of the parent rock by many methods such as the clastic composition analysis, heavy minerals analysis, seismic profile analysis etc. The results indicate that those are mainly controlled by four great sediment source regions, which are from north, east, south and west in the southern Kongdian region. The north provenance is the most important one and can be subdivided into two sub-sources, which are northwest and northeast. Provenance has favorable spatial combination with depositional system. By Dickinson triangular plot of elastic component, most of sands fall in the continental block and volcanic arc, and some in mixed provenance. These results reflect the Huanghua Depression basin is a developed intra-continental rift basin in the Cenozoic, and is featured by the sedimentary characteristics of one-third of obvious and multi-and-near sources in the Mesozoic and Cenozoic tectonic transition process.