1) rich in iron oolite

富铁鲕粒
1.
Systematical studies on the chemical composition,mineral components,characteristics of iron ore and rich in iron oolite in Huoshaoping iron ore are carried out,furthermore the balanced calculations of elements such as Fe,P and so on in ore are dealt with also.
本文系统地研究了火烧坪铁矿石和‘富铁鲕粒’的化学组成、矿物组成及嵌布特征,并对矿石中铁、磷等元素进行了平衡计算。
2) ooide

鲕粒
1.
Study on oil/gas-bearing of lacustrine ooide-limestone of Member 1 of Shahejie Formation in Dongxin Oilfield;
东辛油田下第三系沙一段湖相鲕粒灰岩的含油性
3) oolitic beach

鲕粒滩
1.
The beach body of Lower Triassic Feixianguan Formation in northwestern Sichuan can be divided into platform marginal oolitic beach and intraplatform point beach.
川西北下三叠统飞仙关组滩体分为台地边缘鲕粒滩和台地内点滩2种类型,多数台地边缘鲕粒滩形成时水体相对较深,未经大气淡水和混合水的成岩改造,储集性能较差,局部鲕粒滩形成时水体较浅,在经过大气淡水和混合水的成岩作用改造后,白云石化好,可形成储集性能极好的储集体;台地内点滩白云石化较好,储集性能也较好,但分布狭窄,厚度较薄,无规律可寻。
2.
It is thought that: the reefs are transgressive reefs formed during the regional sea-level rise and vertically mainly distributed in the middle and upper parts of the Changxing Formation, and the oolitic beaches mare mainly regression beaches developed in the process of regional sea-level fall and ver.
本文对四川盆地北部长兴组礁和飞仙关组滩特征和分布及其控制因素作了较为深入的探讨,研究认为生物礁为海平面上升过程中形成的海侵礁,其在纵向上的分布主要位于长兴期中晚期;鲕粒滩主要是在区域海平面下降过程中形成的海退滩,其在纵向上位于飞一—飞三。
4) oolitic limestone

鲕粒灰岩
1.
The confirmation of the oolitic limestones of the Late Carboniferous to the Early Permian Age in the CMB of west Yunnan Province implied the carbonate succession was accumulated in a shallow and agitating environment, possibly as the carbonate caps of oceanic islands.
对昌宁—孟连带晚石炭世至早二叠世碳酸盐岩地层内鲕粒灰岩进行了研究,结果表明,该套碳酸盐岩形成于动荡浅水沉积环境,其成因可能与古特提斯洋内碳酸盐岩洋岛海山有关,并且反映了温暖、较为干燥的古气候背景。
2.
The Cambrian oolitic limestones in the Dabeiwang section in Xuzhou, Jiangsu are characterized by numerous layers,complicated textures and types and diverse morphologies.
徐洲大北望地区寒武系鲕粒灰岩层数众多,结构、类型复杂,形状多样,其中以放射鲕、同心鲕及放射-同心鲕为主。
3.
Through dissolution kinetics experiment under normal temperature and pressure,this paper discussed dissolution kinetics characteristics and morphology evolution of oolitic limestone.
鲕粒灰岩是重要的碳酸盐岩油气储层。
6) oolite deformation

鲕粒变形
1.
Oolite lime of Cambrian Zhangxia group emerged widely in Loucun area north beyond the fault and oolite deformation is widely developed.
断裂带北侧楼村地区广泛出露寒武系张夏组鲕粒灰岩,鲕粒变形普遍发育。
补充资料:钨铁电炉出铁(吉林铁合金厂)
钨铁电炉出铁(吉林铁合金厂)
吻 他排由帕中桩了士朴屏人乙曰“
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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