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泥灰岩

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LST reef characterized by aggradational bioherm or patch reef is generally associated with mixed clastic turbidite, siliceous limestone and mudstones reef.

低水位礁仅发育于台盆背景,以加积丘礁或点礁为特色,常与混屑浊积岩、硅灰岩、硅泥岩共生。

Gray-brown limestone, clay crystal structure, and occasionally rose quartz, conchoidal fracture, thick layered limestone.

灰褐色灰岩,泥晶结构,偶见粉晶,贝壳状断口,厚层状灰岩。

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。

Mottles in leopard limestone have undergone rotational deformation and have certain preferred orientation,while the marly component shows distinct fea- tures of ductile deformation;it is r...

在露头尺度上,豹皮灰岩中的豹斑发生了明显的旋转变形并具有一定的定向性,而泥灰质成分则具有清晰的韧性变形特征,为较典型的碳酸盐糜棱岩;在微观尺度上,构成豹斑的白云石矿物未发生韧性变形,而泥灰质成分中的方解石具有明显的细粒化、拉长和定向。

By 30% replacement of cement with fly ash and LiOH the expansion of concrete microbar with SL limestone is reduced significantly.

为确定以Spratt硅质灰岩和Pittsburg泥质白云质灰岩为代表的两类典型碱活性岩石试体在碱性环境中的膨胀来源和发展评定岩石碱活性的方法,研究了不同条件下SL和PL岩石在砂浆和混凝土中的膨胀行为。

The Dam area is located in Weixi city of YunNan province,whose climate is sub-thermal or the mountain plateau temperate monsoon,the regional water system developed,the exposed strata are mainly limestone、dolomite、schist and phyllite, the aquifer and the Impermeable layers are separated each other.

坝址区位于云南身维西县境内,属亚热-温带季风高原山地天气,区内水系发达,出露的地层主要为泥盆系的灰岩、白云岩及片岩、千枚岩,呈含水层与隔水层互层状构造。

The Neoproterozoic Jiuliqiao Formation in Huainan region is 40-70m thick, consists of sandy, silty and dolomitic limestone.

淮南地区新元古代九里桥组主要由泥质、砂质灰岩和白云质灰岩构成,厚度40—70m。

Several points can be concluded for the area from this paper study:(1) Hydrocarbon mainly occurs in the lower interval of bioclastic limestone and dolomitic limestone(the special lithologic interval ) in Es_1 Member,in which solution pores well developed;(2) Traps are mainly anticlines controlled by f.

本文研究表明,大中旺地区油气主要分布在沙一段下部的生物碎屑灰岩和云质灰岩段,储层溶蚀孔隙发育;圈闭主要为受断层控制的断背斜构造;原油具有高密度、高粘度、中低凝固点、高初馏点、高含硫量和高胶质沥青质等特点,属于未成熟—低成熟油;油源为本地咸水环境下形成的沙一段暗色泥岩。

In these limestones, thin layers of limestone are interbedded with mudstones.

对新疆柯坪地区中奥陶统灰岩和泥岩交互沉积地层中的结核状灰岩的沉积环境和形成机制进行了研究。

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