古地理学报
古地理學報
고지이학보
JOURNAL OF PALAEOGEOGRAPHY
2010年
1期
97-106
,共10页
孟元林%高煜婷%吴河勇%王成%修洪文%张安达%李亚光%姜文亚
孟元林%高煜婷%吳河勇%王成%脩洪文%張安達%李亞光%薑文亞
맹원림%고욱정%오하용%왕성%수홍문%장안체%리아광%강문아
松辽盆地北部%中央坳陷%西部斜坡%东南隆起%大庆长垣%储集层%成岩作用
鬆遼盆地北部%中央坳陷%西部斜坡%東南隆起%大慶長垣%儲集層%成巖作用
송료분지북부%중앙요함%서부사파%동남륭기%대경장원%저집층%성암작용
northern Songliao Basin%Central Depression%Western Slope%Southeastern Uplift%Daqing Placanticline%reservoir%diagenesis
为了研究松辽盆地北部中浅层的区域成岩规律及其影响因素,将该区划分为9个成岩区,分别研究了各成岩区的成岩特征.应用流体包裹体均一温度、镜质组反射率、孢粉颜色指数、色谱-质谱分析、热解分析、有机酸测定、X衍射、普通薄片镜下鉴定、扫描电镜、电子探针、铸体薄片鉴定等资料分别划分了它们的成岩阶段.研究结果表明:松辽盆地北部中浅层的成岩作用具有"东强西弱,古强新弱"的成岩规律;盆地东部的抬升剥蚀幅度大,地温梯度高,成岩作用强;盆地西部的抬升剥蚀幅度小,地温梯度低,成岩作用弱;白垩系泉头组三、四段的地层时代相对较老,在埋深相同的情况下,成岩时间较长,成岩作用相对较强.
為瞭研究鬆遼盆地北部中淺層的區域成巖規律及其影響因素,將該區劃分為9箇成巖區,分彆研究瞭各成巖區的成巖特徵.應用流體包裹體均一溫度、鏡質組反射率、孢粉顏色指數、色譜-質譜分析、熱解分析、有機痠測定、X衍射、普通薄片鏡下鑒定、掃描電鏡、電子探針、鑄體薄片鑒定等資料分彆劃分瞭它們的成巖階段.研究結果錶明:鬆遼盆地北部中淺層的成巖作用具有"東彊西弱,古彊新弱"的成巖規律;盆地東部的抬升剝蝕幅度大,地溫梯度高,成巖作用彊;盆地西部的抬升剝蝕幅度小,地溫梯度低,成巖作用弱;白堊繫泉頭組三、四段的地層時代相對較老,在埋深相同的情況下,成巖時間較長,成巖作用相對較彊.
위료연구송료분지북부중천층적구역성암규률급기영향인소,장해구화분위9개성암구,분별연구료각성암구적성암특정.응용류체포과체균일온도、경질조반사솔、포분안색지수、색보-질보분석、열해분석、유궤산측정、X연사、보통박편경하감정、소묘전경、전자탐침、주체박편감정등자료분별화분료타문적성암계단.연구결과표명:송료분지북부중천층적성암작용구유"동강서약,고강신약"적성암규률;분지동부적태승박식폭도대,지온제도고,성암작용강;분지서부적태승박식폭도소,지온제도저,성암작용약;백성계천두조삼、사단적지층시대상대교로,재매심상동적정황하,성암시간교장,성암작용상대교강.
The northern Songliao Basin was divided into 9 diagenetic districts in order to study the regional diagenetic regularities and the controlling factors of the middle-shallow horizons. The diagenetic characteristics were studied, and the diagenetic stages of the elastic rocks were divided in each diagenetic district using the data of homogenization temperatures of fluid inclusions, Ro, TAI, GC-MS, Rock-Eval, organic acids, XRD, thin section observation, SEM, EPMA, blue epoxy resin-impregnated thin sections. As the results show, the diagenesis of elastic rocks in the eastern part of northern Songliao Basin are more extensive than in the western part of northern Songliao Basin at the same depth because the eroded strata in the eastern part are thicker in the western part, and the thermal gradients of the eastern part are higher than in the western part. Moreover, the diagenesis of the Member 3 and Member 4 of Quantou Formation are more extensive than those of the other strata in the middle-shallow horizons of the basin at the same depth because the Members 3 and 4 are older than the others, and their diagenetic time is longer than those of the others.