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成岩

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The pore structure character of reservoir of Paleogene in Melut Basin of Sudan was analyzed by studying the effect of lithology, diagenesis, pore types and clay minerals on pore structure. This reveals micro-features of the reservoir and its effects on development result. Reservoir lithology is mainly lithic quartz arenite and feldspathic quartz arenite, which has low textural maturity.

从储层的岩性、成岩作用、孔隙类型及影响孔隙结构的因素等方面,对苏丹穆格莱德盆地古近系储层的孔隙结构特征进行了分析,揭示了该储层的微观特征及其对开发的影响。

The stratigraphic trend develops during lithification and is unrelated to any change in the global oceanic δ13C.

地层在成岩作用的同时发生的变化应该与全球海洋δ13C 的变化没有多大的联系。

For example, a rock sample in the lithification domain Fig.

例如,在成岩区域(图1a)样品的同位素数据如下:δ18O =-4‰,δ13C =-3‰。

The relationship between δ13C and δ18O provides a useful means of distinguishing meteoric and burial lithification from marine excursions.

13C和δ18O之间存在的关系提供了一种有效的方法来区分大气水和海洋埋藏成岩之间的波动变化。

1B. In some successions, the isotopic signal is set during lithification in isotopically evolving pore fluids, as discussed above.

某些地层中同时保存了孔隙流体中的同位素变化,这些变化多发生在成岩作用过程。

In Cenozoic rocks, its position in the crossplot would indicate that meteoric waters rich in coastal photosynthetic C were a component of the pore fluids during lithification.

这些新生代的岩石在图1中的位置显示大气水在海岸富集了大量的光合作用碳同位素,这些同位素代表了成岩过程中的孔隙流体的组成。

Rather than indicating C isotope excursions, the Neoproterozoic data seem to represent normal isotope variations that occur during lithification and metamorphism.

这些新元古代样品的数据显示了碳同位素的漂移,但与此同时更表明在成岩和变质作用过程中普通同位素的变化。

2B–f. Instead, they are bounded by the Cenozoic lithification domain to the right, and stream off to lower δ18O values that are readily attributable to later metamorphic alteration.

相反的,这些数据被局限在新生代成岩作用区域左边,氧同位素相对较低的比值可以认为是后期变质交待作用的结果。

The pattern of lithification followed by possible later metamorphism results in a forbidden zone, which contains little data, located to the right of the lithification zone on the isotopic crossplot.

这种成岩作用方式在后期可能经历变质作用,并且最终导致一个不可能达到的区域。

Apparent correlations of low δ13C between widely separated sections may relate simply to eustatic sea-level drops where phreatic lenses intrude simultaneously during lithification.

较低的碳同位素比值出现在了很长期的并且相对独立的沉积其内,表示了这个时期曾经发生过普遍的海水沉降,同时不断出现了潜水区的透镜体的入侵,从而定义为成岩作用。

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他们没有侵略性,但我大喊,并在他们的方向扔石头让他们过的线索,远离我,以防万一。

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在你的书包里槽2把包装纸、数量无关紧要。

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密封,遮光,置阴凉干燥处。