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CHARACTERIZATION OF CLASTIC SEDIMENT: APALYNOFACIES APPROACH

机译:碎屑沉积物的表征:唇面相法

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Palynofacies as a tool for identification of depositional environment is broadly used in oil and gas exploration. Palynofacies study is integrated with palynology study, yet they can stand as independent and separated studies. Many palynofacies applications are presented in geology and one discusses in this paper is characterization of clastic sediment. The origin of organic matters as palynofacies analysis objects and its classifications is actually the first step in characterization of clastic sediment.Sample of sediment are characterized by the absolute and relative proportion of structureless amorphous material, dinoflagellate cyst, foraminiferal test lining, resin, black debris, yellow brown fragment, dark brown fragment, cuticle, plant tissue, woody material, pollen, spore and fungal and relative proportion as mentioned by Tyson (1995).Recently, palynofacies trends can be related to sequence stratigraphy in order to provide an outline of predictive model for more detailed investigations.
机译:作为用于鉴定沉积环境的工具,帕尔恰诺瓦斯广泛用于石油和天然气勘探。 Palynofacies研究与Palynology研究相结合,但它们可以成为独立和分开的研究。许多野生遗传应用呈现在地质学中,本文中的一个讨论是碎屑沉积物的表征。有机物的起源是帕锡分析对象及其分类实际上是碎屑沉积物表征的第一步。 沉积物样品的特征是由结构无定形材料,丁胺酸纤维素囊肿,多胺类试验衬里,树脂,黑碎片,黄褐色片段,深褐色片段,角质层,植物组织,木质材料,花粉,孢子和真菌和真菌和真菌和真菌和真菌的绝对和相对比例的特征泰森(1995)提到的相对比例。 最近,帕锡缺陷趋势可能与序列地层有关,以便为更详细的调查提供预测模型的概要。

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