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carbonate rocks相关的网络例句

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与 carbonate rocks 相关的网络例句 [注:此内容来源于网络,仅供参考]

For a wide variety of lithologies from granite through gneiss, carbonate and amphibolite to basaltic rocks, it is shown that this relation is valid in the range 0~350 API and 0.03~7μW/m3 respectively with an error lower than 10%.

从片麻岩、碳酸盐岩、角闪岩、花岗岩到玄武岩,在这样宽的岩性变化范围内,显示出这种线性关系在0~350 API和0.03~7 μW/m3范围是有效的,其误差均小于10%。

But the genesis of the carbonite reservoir rocks, the differences in lithology, diagenesis, post diagenesis, structural fractures and dissolution have made it difficult for the general concepts and methods of the flow units to be suitably used in fracture-and-cavernous carbonate reservoirs.

主要储集空间以构造变形产生的构造裂缝与岩溶作用形成的孔、洞、缝为主,其中大型洞穴是最主要的储集空间,裂缝既是主要的储集空间,也是主要的连通通道。塔里木盆地塔河碳酸盐岩油田即属于此类油藏。

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。

These rocks are known as the Cathedral Formation, and probably represent the escarpment of a large submarine slump like those observed off the edge of carbonate platforms in areas like the Bahamas and Honduras today.

这些岩石被称为大教堂的形成,并可能代表绝壁一个大的潜艇衰退一样观察了边缘的碳酸盐平台等领域的巴哈马和洪都拉斯今天。

Most source rocks of the large marine oil-gas fields in domestic and overseas are graptolite shale, oil shale and marl with great amounts of clay mineral, which formed in the deepwater slope environment transferred from tableland to trough.But the carbonate rock is formed in the shallow water environment under good exchanging condition with atmosphere, which causes the low abundance of organic matter and poor-type kerogen.

国内外海相大油气田的烃源岩多为黏土矿物含量较高的泥页岩、油页岩和泥灰岩,形成于由台地向海槽过渡的深水斜坡环境,而碳酸盐岩形成于与大气交换条件较好的浅水环境,是有机质丰度低和干酪根类型差的根本原因。

Heritage include: geological sites, glorious carbonate洞顶and ground, the pure black lava wall and regarded as the most perfect lava cave system; sunrise peak posed by the tuff cone-shaped mountain, as tall as the fortress seaside, stunning scenery; peak Korea - Han Mt to waterfalls, rocks and different form of crater lakes and famous.

遗产包括:地质遗址,绚丽多彩的碳酸盐洞顶和地面,纯黑色的熔岩洞壁,被视为最完美的熔岩洞窟体系;日出峰,由凝灰岩构成的锥形山峰,如堡垒般矗立在海边,景色令人叹为观止;韩国最高峰——汉拿山,以瀑布、形态各异的岩石和火山口湖泊而闻名。

The mineralization of gold and silver is zoned and closely related to silicification of carbonate and clastic rocks, so siliceous ore dominates in the deposit.

矿化温度主要在300~170 C之间,成矿流体的主要成分为K~-、Na~-、Ca~(2+)、Mg~(2+)、Cl~。金属配合物的分配计算显示,金在成矿热液中主要以疏氢配合物迁移,而银、铁、铅、锌则以氯配合物为主,铁、铅、锌在成矿后期的中性-弱碱性环境下可转变为羟基和硫氢配合物。

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。

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