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碳酸盐岩

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The structural mélanges is of the shape of a trumpet with its west section more wide and its east section more narrow, being made up of flysch slice, archibathyal silicalite, argillite slice, serpentinite slice, island arc slice, carbonate rock slice, continent-breaken pieces and so on.

该带西宽东窄,呈喇叭状,由复理石岩片、深海硅质岩、泥质岩岩片、蛇纹质岩片、火山岛弧岩片、碳酸盐岩岩片、大陆碎片岩片等组成。其中以复理石岩片为基质包含其它外来构造岩片。

Thus, microbial carbonates should be classified within the limestones. Similar to reef rocks, microbial carbonates are frequently developed in strata from the Precambrian through to the Phanerozoic, in three forms: reef, biostrome and bioherm.

微生物碳酸盐岩,总体上构成生物作用类碳酸盐岩中的粘结岩类,以其明显的微生物作用特点而具有自己的分类体系;它不但作为生物礁岩石的主要类型,而且也常常以生物礁、生物层和生物丘三种形式发育在地层之中。

Microspar structures carbonate is characterized by elphent tooth-like structure consisting of fine, equant sparry calcite crystals, and hosting rocks is mainly fine-grained carbonates with mud.

臼齿构造碳酸盐岩是一种具有类似于大象臼齿特征的特殊碳酸盐岩,其微亮晶脉由纯净的、基本等粒的方解石构成,而基质物质则由细粒的、富泥质的灰岩组成。

Microspar structures carbonate is characterized by elphent toothlike structure consisting of fine,equant sparry calcitecrystals,and hosting rocks is mainly finegrained carbonates with mud.

臼齿构造碳酸盐岩是一种具有类似于大象臼齿特征的特殊碳酸盐岩,其微亮晶脉由纯净的、基本等粒的方解石构成,而基质物质则由细粒的、富泥质的灰岩组成。

As the aeolotropism development of cracks in carbonate reservoir, so far not a very good seismic reservoir crosswise prediction method application for the aeolotropism carbonate reservoir, especially in the seismic, logging joint inversion, is mainly continues to use the reservoir crosswise prediction method that suitable for the isotropic clastic rock reservoir.

由于碳酸盐岩储层裂缝发育的非均质性,到目前为止还没有一套推广应用很好的针对碳酸盐岩非均质性储层进行地震储层横向预测的方法,尤其是在地震、测井联合反演方面,主要是沿用适合于较均质的碎屑岩储层地震横向预测技术。

Mature, synrift lacustrine shales of Eocene to Oligocene age and mature, late rift coals and coaly shales of Oligocene to Miocene age are source rocks for oil and gas in two important petroleum systems of the onshore and offshore areas of the Northwest Java Basin. Biogenic gas and carbonate sourced gas have also been identified. These hydrocarbons are trapped primarily in anticlines and fault blocks involving sandstone and carbonate reservoirs.

爪哇盆地西北的沿海地区的两个重要的石油体系中,始新世至渐新世的湖泊页岩、渐新世至中新世晚期裂隙煤和含煤页岩是石油和天然气的矿源岩,鉴别出了生物源气体和碳酸盐源气体,这些烃类被圈闭在背斜和断层中,包括沙岩、碳酸盐岩油储。

Sequential leaching experiments indicate fluorine in carbonate rock, phosphorite and Mo-Ni ore layer occurs principally in dissolvable forms: water-soluble, associated with carbonate or phosphorite, so fluorine in which rocks have high chemical mobility at surface conditions. Fluorine in siliceous rock, black shale and carbonaceous slate mainly occurs in undissolvable forms, which are inert at surface conditions.

氟在碳酸盐岩、磷块岩、钼、镍等多元素富集层及部分硅质岩中主要以水溶态、碳酸盐结合态等易溶形式存在,其在自然条件下的化学活动性强;而氟在碳质板岩、黑色页岩及大部分硅质岩中主要存在于难溶矿物中,其化学活动性较弱。

The exposed massive cold-seep carbonates provided substrate for the encrustations of corals as well as coralline algae and might have played a crucial role in the initial development of coral reefs in a siliciclastic paleoenvironment of active tectonic setting. This is probable the first case of the world that cold-seep carbonates acting as initial colonization hardgrounds of hermatypic corals and corallines.

在此基底泥岩快速浅化的过程中,出露的块状冷泉碳酸盐岩成为不稳定地体构造背景中,珊瑚与珊瑚藻等表覆生物在矽质碎屑环境生长的硬底质,可能在礁体的最初发育扮演关键性的角色;此种冷泉碳酸盐岩成为造礁珊瑚与珊瑚藻在矽质碎屑古环境中最初生长硬底质的现象,很可能为世界首例。

In this aspect the amount of acid-insoluble residues in the dolomites is one of the important factors controlling weathering and pedogenesis of carbonate rocks.

这一方面为反映出白云岩中&不溶物&的多少是制约着碳酸盐岩区成土的一个重要因素,同时也为碳酸盐岩区石漠化提供理论基础。

When the sandstones are surrounded by carbonates or thick mudstones, then high carbonate contents will be found in the sandstones.

当砂岩层围岩为碳酸盐岩或厚的泥岩时,在砂岩层内部易形成高碳酸盐含量、胶结作用强烈的含碳酸盐胶结物。

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