1) biogenetic rock
生物岩
2) 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。
3) 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
['baiəu,hə:m]
生物礁岩
5) biokarst
生物岩溶
1.
Through biochemical and physical processes, they bore and corrode the substrate, thus producing distinct biokarst microforms.
并讨论和展望了生物岩溶微形态研究的前景,开拓生物岩溶研究新思路。
2.
The paper discusses the types and formation mechanisms of the erosional products of biokarst on limestione in Guilin area.
桂林岩溶区石灰岩表面生物岩溶溶蚀形态可分为四类:(1)微溶孔,包括壳状内生地衣微溶孔和藻类微溶孔;(2)溶孔,藻类成因的口小腹大的囊袋状溶蚀;(3)溶坑,藻类、地衣、苔藓及腐殖土成因的柱状、锥状、半球状溶蚀;(4)溶盆,各类生物及腐殖土共同作用而成的壁陡底平的盆状溶蚀。
6) microbialite
微生物岩
1.
Age and sedimentology of microbialites after the end-Permian mass extinction in Luodian,Guizhou Province;
贵州罗甸二叠纪末生物大灭绝事件后沉积的微生物岩的时代和沉积学特征
2.
Abundant microbialites,from the Middle Cambrian Qinjiamiao Group in the Gudongkou section near Xingshan County of Hubei Province,south China,were studied and described in detail by macro-and microscopic observations.
通过野外考察及对岩石光面的观察,发现湖北兴山古洞口剖面中寒武统覃家庙群微生物岩的类型主要为波状-半球状叠层石,少量为凝块石。
3.
This paper refers to a 3 m thick microbialite in the Permian-Triassic boundary section in Laolongdong, Chongqing.
剖面研究揭示,重庆老龙洞地区二叠系—三叠系界线上下地层中发育厚约3m的微生物岩。
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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参考词条