1) biolithite
[,baiəu'liθait]

生物灰岩
1.
Reservoir body study and cognition for lower Sha 1 biolithite of Zhouqingzhuang area;

周清庄地区沙一下生物灰岩储集体研究与认识
2.
An integrated study on biolithite reservoir in Wangxuzhuang oil field;

王徐庄油田生物灰岩储集层综合研究
3.
The lacustrine carbonate rock in Member 1 of Shahejie Formation, Dongxin Oilfield, composes mainly of biolithite and ooides limestone as well as a few ancylus fluviatilis limestone, and is developed in a real favorable position for oil and gas migration and accumulation with great resources potential.
东营凹陷东辛油田沙一段湖相碳酸盐岩以生物灰岩及鲕粒灰岩为主,处于油气运聚非常有利的位置,资源潜力巨大。
2) Biolimestone

生物灰岩
1.
The Distribtion of Biolimestone and Igneous Rock in Dagang Area and the Research for Its Hydrocarbon Reservoir;
大港地区生物灰岩和火成岩的分布及其油气藏的研究
2.
The thin biolimestone was an important petroleum exploration area that was ignored in continental deposit basin.
陆相湖盆中的薄层生物灰岩是一个被忽视的油气勘探的重要领域。
3.
In the west slope of Jinhu Depression in Jiangsu Basin,E1f2 biolimestone reservoir was small in overall thickness,uneven areal distribution,fast lateral change,high thickness difference,thus the reservoir thickness was hard to be recognized by conventional seismic description.
苏北盆地金湖凹陷西斜坡阜二段生物灰岩储层总体厚度薄,平面分布不均,横向变化快,厚度差异大,常规地震解释很难有效识别储层厚度。
4) bioherm limestone

生物礁灰岩
1.
Shasiduan bioherm limestone gas reservoir in Ping-fangwang area is the largest uncompartmentalized oilfield in Shengli oilfield with proved reserves of 164.
储层是以复礁体为特征的生物礁灰岩,其突出特点表现为平面与层内的非均质性,总体上看,含气构造轴部的渗滤能力比两翼强。
5) biogenetic limestone

生物石灰岩
6) bioclastic limestone

生物碎屑灰岩
1.
By researching pyrolyzed gas generated by hydropyrolyzed bioclastic limestone from lacustrine facies in Pingyi basin, Shandong Province, the evolution characteristics of yields, compositions and structure parameters of pyrolyzed gas are discussed.
通过对山东平邑盆地下第三系湖相生物碎屑灰岩加水热模拟气的研究,探讨了热解气的产率、组成及结构参数的变化特征。
2.
According to the features of thin layer and quick changes in spatial of bioclastic limestone in the western ramp of Qikou depression,the lower Es1 member of Shahejie formation was divided into three .
针对该地区沙一下亚段储层单层厚度薄、横向岩相变化快的特点,首先采用沉积旋回分析法将所研究的目的层划分出3个五级高频旋回层序,并归纳了岩相序列模式;再利用有色反演沿层切片法,检测出薄互层地层中高波阻抗体的形态及其在时间域上的变化;最后以岩相序列模式分析法解释反演结果,实现了五级高频旋回层序内的岩相重构,最终预测出该地区沙一下亚段厚度为3~9m的生物碎屑灰岩薄储层的平面分布,达到了储层分布预测的目的。
补充资料:化工灰岩矿
分子式:
CAS号:
性质:一种以方解石为主要矿物组分的非金属矿产。常含少量的白云石、菱镁矿等。包括电石灰岩和制碱灰岩。化工灰岩矿一般品位指标见表。用露天开采法,一般不选矿或用洗选法处理。用于制造碱、电石、轻质碳酸钙,还可用作催化剂、漂白粉、钙质饲料及其他化工原料。项 目电石灰岩(以氧化钙计)/%制碱灰岩(以碳酸钙计)/%边界品位5288工业品位5490
CAS号:
性质:一种以方解石为主要矿物组分的非金属矿产。常含少量的白云石、菱镁矿等。包括电石灰岩和制碱灰岩。化工灰岩矿一般品位指标见表。用露天开采法,一般不选矿或用洗选法处理。用于制造碱、电石、轻质碳酸钙,还可用作催化剂、漂白粉、钙质饲料及其他化工原料。项 目电石灰岩(以氧化钙计)/%制碱灰岩(以碳酸钙计)/%边界品位5288工业品位5490
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