鄂尔多斯盆地南缘岐山剖面中奥陶统平凉组沉积环境分析

Sedimentary environments of the Middle Ordovician Pingliang Formation in the Qishan section, southern Ordos Basin

关键词:  鄂尔多斯盆地  岐山剖面  中奥陶统  平凉组  沉积环境

Key words:  Ordos Basin  Qishan section  Middle Ordovician  Pingliang Formation  sedimentary environment

摘要:

鄂尔多斯盆地南缘岐山剖面平凉组以碎屑岩和碳酸盐岩混积为特征,根据岩性特征可将平凉组分为七段。其中碎屑岩约占80%,主要分布在平一、三、五、七段;碳酸盐岩约占20%,主要分布在平二、四、六段。研究表明,岐山剖面平凉组属于大陆斜坡环境,是一套多旋回沉积,其中一-二段、三-四段、五-六段分别构成一个海进海退旋回,属于上斜坡-下斜坡交互沉积环境,第七段单独构成一个海进旋回。至唐陵组初期,海水开始退去。

Abstract:

The Middle Ordovician Pingliang Formation strata well-developed and outcropped in the Qishan section, Baoji, Shaanxi are interpreted to be an ideal section for the study of the Ordovician marine strata in the Ordos Basin. The Pingliang Formation may be divided into seven lithologic members. The clastic rocks make up about 80 per cent, and are organized dominantly in the 1st, 3rd, 5th and 7th members of the Pingliang Formation. The carbonate rocks occupy the other 20 per cent, and constitute the 2nd, 4th and 6th members of the Pingliang Formation. The Pingliang Formation in the Qishan section is assigned to the continental slope environment and consists of a succession of polycyclic deposits. The 1st to 2nd, 3rd to 4th, and 5th to 6th members are grouped into three transgressive-regressive cycles, respectively, and laid down in the transitional environments of the upper continental and lower continental slopes. The 7th member is made up of a single transgressive cycle, and the regression in this member occurred at the onset of the deposition of the Tangling Formation.