首页> 外文期刊>Journal of Geoscience and Environment Protection >Petrology Characters of Conglomerates in Baikouquan Formation, Mahu Sag, Junggar Basin
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Petrology Characters of Conglomerates in Baikouquan Formation, Mahu Sag, Junggar Basin

机译:准gar尔盆地麻湖凹陷百口泉组砾岩的岩石学特征

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Mahu Sag, one of the most oil and gas bearing sags in Junggar basin, is in the northwestern margin of the basin. On gentle slope region of the sag, a serial of large scale coarse fan delta deposits were developed in Triassic Baikouquan Formation. In order to understand the petrology characters of conglomerates in Baikouquan Formation, based on lots of cores, grain size analysis, normal thin sections, casting thin sections, scanning electron photomicrographs, mineral composition identifications, clay mineral and bulk composition identifications of X-ray diffraction, were comparatively studied for Xiazijie and Huangyangquan fan-delta in Mahu Sag. Mineral composition of conglomerates is main tuff, while eurite, dacite, rhyolite, andesite and granite are common. However, more tuff and granite, less eurite and andesite in Xiazijie fan-delta, there is no rhyolite in Huangyangquan fan-delta. Kaolinization and chloritization of conglomerates are ubiquitous in the formation. The content of chlorite and kaolinite is higher in Xiazijie fan-delta, with lower illite-smectite and illite. There is less feldspar of clastic and more calcite of cement in Xiazijie fan-delta.
机译:玛格凹陷是准gar尔盆地含油气最多的凹陷之一,位于盆地西北缘。在凹陷的缓坡区,三叠系白口泉组发育了一系列大规模的粗扇三角洲沉积物。为了了解百口泉组砾岩的岩石学特征,基于大量岩心,粒度分析,正常薄片,铸件薄片,扫描电子显微照片,矿物成分鉴定,粘土矿物和X射线衍射的体成分鉴定对马虎凹陷下子街和黄阳泉扇三角洲进行了比较研究。砾岩的矿物成分是主要凝灰岩,而堇青石,钠铁矿,流纹岩,安山岩和花岗岩是常见的。下子街扇三角洲的凝灰岩和花岗石较多,较少的绢云母和安山岩,而黄阳泉扇三角洲没有流纹岩。砾岩的高岭土化和氯化是无处不在的。下子街扇三角洲绿泥石和高岭石含量较高,伊利石-蒙脱石和伊利石含量较低。下子街扇三角洲碎屑长石较少,水泥方解石较多。

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