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Oil Sands Forming Model and Character in the Northwest Edge of the Junggar Basin, China

机译:在中国准噶尔盆地西北边缘的石油砂形成模型和性格

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The Junggar Basin has the basic conditions for giant oil-sand mine to form and it is the hot point for exploration & development of oil sands. Multi-layer source rocks deposited in The Manas Lake Depression have produced abundant hydrocarbon in the course of multi- phase tectonic movement and they were the source of oil sands. Many unconformities formed also in the course of multi-phase tectonic movement were the main pathway of lateral movement of hydrocarbon and the welldeveloped abnormal faults were the main vertical pathway. The sands bodies of fluvial facies in alluvial fans in front of the Zhair Mountain offered a very favorable reservoirs for oil-sand mine. Hard biodegradation make the viscosity of hydrocarbon heavier and heavier. The hydrocarbon seized on the surface of sands, and then oil sands were formed. The peculiar characters of the northwest edge of the Junggar Basin make the oil sands occur at the compressive side of the basin. And the lateral distribution of oil sands mine is bigger and the scale is smaller relatively. The fault' openness, fossil landscape, sedimentary facies, oil viscosity etc. have controlled the abundance and distribution of oil sands.
机译:Junggar Basin拥有巨型油砂矿的基本条件,是勘探开发油砂的热点。沉积在玛纳斯湖​​凹陷中的多层源岩在多相构造运动过程中产生了丰富的碳氢化合物,它们是油砂的源泉。在多相构造运动过程中也形成的许多不整合是烃的横向运动的主要途径,并且威力的异常断层是主要的垂直途径。 Zhair Mountain前面的冲积球迷中河的沙子尸体为油砂矿提供了一个非常有利的水库。硬生物降解使烃的粘度更重,更重。在沙子表面上捕获的烃,然后形成油砂。准噶尔盆地西北边缘的特殊特征使油砂发生在盆地的压缩侧。而油砂矿的横向分布较大,比例相对较小。故障“开放性,化石景观,沉积相,油粘度等控制了油砂的丰富和分布。

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