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Study on the phosphorate minerals assemblage shows that strongly developed anatexis of the area is responsible the occurrence of wagnerite and its coexistence with apatite, and both present as rock-forming minerals. The volatiles F, P and components Ca, Mg determine the formation of wagnerite, while the P-T condition affects the variation of wagnerite polytypes.

通过磷酸盐矿物组合的岩石学研究得知强烈发育的深熔作用导致氟磷镁石与磷灰石共生并以造岩矿物出现,挥发分F、P以及Ca、Mg等成分因素决定氟磷镁石的出现与否、温压条件控制氟磷镁石的多型变化。

It mainly reaches the following achievements:1 Through the research of petrology and geochemistry, it is found that dunite takes over 85 percent in ultramafic intrusion, which largely contains Mg(39.66%-47.20%) and Fe(733%-11.17%). The containing of Mn. K. Na, P and Ti is less than 0.1 percent respectively. So it has typical characteristic of leaving of mantle rocks, while it doesnt have partly characteristic of melting.

主要取得以下认识: 1 通过对超镁铁质岩体的岩石学、地球化学研究发现,松树沟超镁铁质岩体主要由纯橄榄岩和方辉橄榄岩组成,纯橄榄岩占85%以上,变质浅,变形相对简单,富含Mg(39.66%—47.20%)和Fe(7.33%—11.17%),Mn、K、Na、P和Ti的含量通常都低于0.1%,具有明显的地幔岩残留体性质,而不具有部分熔融的特征。

After many studies on geochronology, geochemistry and petrology of the eclogite from Bixiling have been done, its formation and metamorphic history are well known now.

根据大量年代学、地球化学和岩石学等方面的研究,前人对碧溪岭榴辉岩的形成及变质历史有了较明确的认识,但这些研究对超高压变质前后过程中元素和同位素的变化涉及较少。

This paper, based on previous data, detailed core observation and petrology features, puts forward that member 1 of Shanxi Formation represents marine facies or the marine-continental transition depositional environment, such as ①high maturity of the component and texture squartz-sandstone,②micrite siderite stone,③sea lily, foraminifer mudstone,④bauxite mudstone and ⑤crystal powder dolomite.

在前人大量研究基础上,通过详细的岩心观察和岩石学特征的分析,在山西组一段发现了代表海相或海陆过渡环境沉积的典型特征,分别为①成分成熟度和结构成熟度均高的石英砂岩、②泥晶菱铁矿岩、③海百合、有孔虫骨屑泥岩、④铝土矿质泥岩和⑤粉晶白云岩。

Firstly, based on the observation and description of a large number of drilling cores in macroscopic and microcosmic aspects, facies marks are summarised, which supplied from the characteristics of lithology, distribution of grain size, sedimentary structvure, ichnology and logging facies.

首先,在对大量岩心宏观和微观特征描述的基础上,从岩石学特征、粒度分布特征、沉积构造特征、遗迹化石特征以及测井相特征等五方面,总结出研究区的各类沉积相的相标志,为沉积相的识别和划分提供了有力的依据。

Beginning with petrology analysis of reservoirs, this paper introduces the causes of 4 kinds of sensitivities of sandstone reservoirs and their functional principles.

从油气储层岩石学分析入手,阐述了砂岩储层4类敏感性发生的原因及作用机理,结合几个实例,论述了油气开发实践中,必须针对砂岩储层的非均质性特点,对症下药,在充分掌握储层伤害机理的基础上,研制保护与改造油气层的措施,才能取得实效。

The petrology of the Cenozoic volcanic rocks and their distribution in the Liaohe basin indicate a continental rift environment;The uparching of the upper mantle revealed by geophysical data has controlled the development of the structures on the surface.

辽河盆地新生代火山岩的分布规律和岩石学特征表明:辽河盆地新生代的构造环境为大陆裂谷。地壳深部资料显示出辽河地区存在上地幔隆起,它控制了浅部构造的发育。

The extinction of the two-pyroxene-bearing granulites within the temperature range higher than 950℃ indicates the position of petrological crust-mantle boundary beneath Hannuoba area.

二辉二长麻粒岩落在相似的温压范围内。麻粒岩捕掳体在950℃处的突然消失指示了第三纪时汉诺坝地区岩石学壳幔边界的温度。

On the basis of the researching of facies、 petrology、 cathodoluminescence analysis, this paper concludes that the terrigenous clastics in Pingyipu Formation were mostly originated from Motianling palaeo-peninsula lied to its north, and sands in distributary channels、 braidedriver in estuaries、 deltas and in littoral zone in hybrids could be derived from Middle-Sichuan Palaeoland with Peng-Guan Highland.

对早中泥盆世浑水陆源碎屑沉积及混合沉积的沉积相、岩石学、阴极发光等研究分析,作者推测,该区陆源碎屑主要来自北边的摩天岭古半岛,而分流河道、辫状河充填及混积滨岸砂则可能以川中古陆和彭灌高地为主要源区。这一点与过去通常认为的主要来自彭灌岛和轿子顶古岛差别较大。

The petrography and mineral chemistry characteristics of the two spinel-rich spherules show features of crystallization from liquids and their alteration taken place under non-oxidized surrounding.

岩石学和矿物化学特征表明,GRV 020025-3RI8和GRV 021579-3RI5都经历过熔融结晶过程,它们的蚀变均发生在非氧化的含水或无水的环境中。

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