现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2014年
3期
635-644
,共10页
刘永福%赵建华%范秋海%林畅松%孙琦%黄理力
劉永福%趙建華%範鞦海%林暢鬆%孫琦%黃理力
류영복%조건화%범추해%림창송%손기%황리력
东河砂岩%成岩作用%沉积相%埋藏作用%层序地层%沉积速率
東河砂巖%成巖作用%沉積相%埋藏作用%層序地層%沉積速率
동하사암%성암작용%침적상%매장작용%층서지층%침적속솔
Donghe sandstone%diagenesis%sedimentary facies%burial%sequence stratigraphy%deposition rate
通过岩心及薄片的观察,结合扫描电镜阴极发光等资料分析,对哈拉哈塘地区东河砂岩成岩作用进行了研究。结果表明:东河砂岩以岩屑石英砂岩为主,成岩作用类型有压实作用、胶结作用、溶解作用及交代作用。综合成岩作用的组合类型及其演化序列,认为本区东河砂岩主体处于中成岩阶段A期。分别讨论了沉积相、埋藏作用和层序地层等对成岩作用的控制,研究区东河砂岩在低温背景下,长期浅埋且晚期短暂快速深埋,总体上压实程度中等;主要发育滨岸和浪控三角洲沉积体系,在高精度层序界面附近,相对海平面上升,可容纳空间增大,沉积物沉积速率相对较低,且停留时间长,在同生成岩和早成岩阶段容易形成广泛分布的碳酸盐胶结。
通過巖心及薄片的觀察,結閤掃描電鏡陰極髮光等資料分析,對哈拉哈塘地區東河砂巖成巖作用進行瞭研究。結果錶明:東河砂巖以巖屑石英砂巖為主,成巖作用類型有壓實作用、膠結作用、溶解作用及交代作用。綜閤成巖作用的組閤類型及其縯化序列,認為本區東河砂巖主體處于中成巖階段A期。分彆討論瞭沉積相、埋藏作用和層序地層等對成巖作用的控製,研究區東河砂巖在低溫揹景下,長期淺埋且晚期短暫快速深埋,總體上壓實程度中等;主要髮育濱岸和浪控三角洲沉積體繫,在高精度層序界麵附近,相對海平麵上升,可容納空間增大,沉積物沉積速率相對較低,且停留時間長,在同生成巖和早成巖階段容易形成廣汎分佈的碳痠鹽膠結。
통과암심급박편적관찰,결합소묘전경음겁발광등자료분석,대합랍합당지구동하사암성암작용진행료연구。결과표명:동하사암이암설석영사암위주,성암작용류형유압실작용、효결작용、용해작용급교대작용。종합성암작용적조합류형급기연화서렬,인위본구동하사암주체처우중성암계단A기。분별토론료침적상、매장작용화층서지층등대성암작용적공제,연구구동하사암재저온배경하,장기천매차만기단잠쾌속심매,총체상압실정도중등;주요발육빈안화랑공삼각주침적체계,재고정도층서계면부근,상대해평면상승,가용납공간증대,침적물침적속솔상대교저,차정류시간장,재동생성암화조성암계단용역형성엄범분포적탄산염효결。
Donghe sandstone diagenesis were studied through core and rock slice observations and data analysi-ses of scanning electron microscope and cathodoluminescence in the Hanilcatam depression.The reservoir rocks mainly is lithic quartz sandstone.The types of the diagenesis are the compaction,cementation,replacement and dissolution.The diagenetic stage belongs to the A middle diagenesis.The control of sedimentary facies,burial and sequence stratigraphy on diagenesis are discussed.Donghe sandstone in the study area was long-term shal-low buried and short-term quick deep buried in later period in the low-temperature background,so the degree of compaction is moderate in general.Shore and wave-dominated deltaic depositional systems are developed.Near the high-resolution sequence boundaries where relative sea-level rises,accommodate space increases,sediment deposition rate is relatively low,and residence time is long,develop laterally persistent carbonate cemented ho-rizons in syndiagenesis and early diagenesis stages.