鲁西南二叠纪近海盆地缓坡三角洲沉积古地理演化
Permian Paralic Basin Sedimentary Paleogeographic Evolution of Gently Dipping Delta in Southwestern Shandong
别立珍
摘要(Abstract):
运用沉积学、岩石学的方法,结合野外露头实测与钻井观察,在鲁西南二叠纪近海盆地缓坡三角洲沉积中识别出6种岩相和8种沉积微相,其中6种岩相为灰黄色粗砂岩相(CS)、浅灰色中砂岩相(MS)、浅灰色细砂岩相(FS)、深灰色互层的泥岩与粉砂岩相(MFS)、煤(CB)、暗色泥岩相(DM);8种沉积微相为分流河道相(MS与CS相组合)、河口砂坝相(MS与FS相组合)、天然堤相(FS与MFS相组合)、决口扇相(MS、FS与MFS相组合)、分流间湾相(DM与MFS相组合)、泥炭沼泽相(DM与CB相组合)、远砂坝相(MFS)和海湾或滨浅海相(DM)。在此基础上,采用层序地层方法进行等时地层对比,发现本区三角洲沉积序列含有4个沉积旋回,C1旋回早期以前三角洲的海湾相为主,晚期为三角洲前缘和三角洲平原沉积;C2旋回早期以三角洲前缘、前三角洲和三角洲平原沉积为主,晚期为三角洲平原沉积;C3旋回早期为三角洲前缘沉积,晚期为三角洲平原沉积;C4旋回主要以三角洲平原为主和陆相的河流沉积。
关键词(KeyWords): 鲁西南;二叠系;三角洲;古地理
基金项目(Foundation):
作者(Author): 别立珍
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