The Karamaili ophiolite complex in East Junggar of Xinjiang province was composed of metamorphic peridotite, gabbro, diabase and basic lava. 新疆东准噶尔卡拉麦里蛇绿混杂岩的岩石组合为变质橄榄岩、辉长岩、辉绿岩和基性熔岩等。
Late Permian Diabase in Luodian, Southeastern Guizhou, and Its Tectonic Significances 贵州罗甸晚二叠世辉绿岩及其区域构造意义
A mottled green rock composed of diabase. common serpentine 绿色蛇纹石含有辉绿岩并带有花纹的绿色岩石
The gold deposit is located in the contact zones of diabase and strata, which are strictly controlled by the contact zones and the compressed fragmentized belts. 该矿产于辉绿岩体与地层的接触带,严格受接触带和挤压破碎带的共同控制。
The diabase dike group is developed in metamorphic basement in Zhulou Mountain at the South Edge of Jiuling Mountain, their forming era and their origins have not been researched. 九岭南缘安义珠洛山变质基底地层中也发育有辉绿岩岩墙群,其形成时代及成因未作过研究。
Experimental research on reinforcement effect of compound grouting on diabase dikes 辉绿岩脉复合灌浆试验加固效果研究
Using diabase fiber instead of glass fiber reinforce PVC in order to resolve the difficult process problem. 本文首次对高强度、高刚度、低成本的辉绿岩纤维增强PVC复合材料进行了研究。
A dark, fine-grained igneous rock; diabase. The amphibolite and basic granulite may be comparable to the world's metamorphic tholeiite. 粗玄岩,辉绿岩一种暗色微粒火成岩;辉绿岩斜长角闪岩和基性麻粒岩可与世界变质拉斑玄武岩对比。
The NWW-extending Cretaceous amphibolic diabase dikes are developed in Xiazhuang uranium ore field, Northern Guangdong province. 下庄铀矿田北西西向分布的白垩纪角闪辉绿岩构成区内基性脉岩的主体。
Diabase connected depth and shallow and caused deep auriferous metallogenetic fluid through rifted fractured zone uplifting and precipitation. 辉绿岩起着沟通深部与浅部构造,并使深部的含矿流体沿挤压破碎带上升、沉淀而成矿的作用。
The volcanic rock series in the Rucheng basin in southeastern Hunan is composed of the basalt, diabase and basaltic pyroclastic rock. 湘东南汝城盆地火山岩系由辉绿岩、玄武岩和玄武质火山碎屑岩组成,属于低钾拉斑玄武岩系。
Influence of diabase intrusion on hydrocarbon generation of depositional organic matter 异常地热对沉积有机质生烃过程的影响&以辉绿岩侵入体为例
The temperature of brittle ductile transition of dry gabbro is 100 ℃, higher than that of dry diabase. 干的辉长岩样品比干的辉绿岩样品发生脆延性转化的温度高100℃;
Preparation of the diabase gravel and performance of concrete were studied for the demand of freeway. 结合高速公路的建设需要,对辉绿岩碎石制备及其混凝土的性能进行了研究。
The diabase, lamprophyre, granite porphyry and quartz veins are formed after Variscan period. 辉绿岩、煌斑岩、花岗斑岩及石英脉形成于华力西期以后。
It was investigated that the effects of the diabase aggregate and limestone aggregate on the workability and compressive strength and the property of interfacial transition zone ( ITZ) of aggregate-cement. 测试了辉绿岩碎石和石灰石碎石作集料对混凝土工作性、强度以及界面特性影响。
Research on artificial diabase aggregate and powder and utilization 辉绿岩人工砂石粉的研究与利用
Property test and study for RCC of artificial diabase sand mixed with fluvial sand 辉绿岩人工砂掺河砂碾压混凝土性能试验研究
Two micro-disseminated gold deposits existed in diabase in Northwest Guangxi province were discovered, The deposits are controlled by faults structure and diabase, the later formed the host rock. 在桂西北地区新发现了两个直接产于辉绿岩中、以辉绿岩为赋矿主岩的微细浸染型金矿床(点)。金矿床受断裂构造和岩性控制,含矿岩石为蚀变辉绿岩。
Fushan Iron Mine introduced diabase cast stone pipes in its concentrator instead of steel piplcs which have quicker wear. 为了解决选矿厂钢管道磨损快的问题,符山铁矿选矿厂采用了辉绿岩铸石管道,经使用证明,铸石管道的磨损仅为普通钢管6%。
This paper has studied the Cenozoic diabase dike swarm, character of basalt eruptions, structures of basins and grabens, rheological feature of peridotite inclusions in the basalt and fault striations. 本文研究了漳州&厦门地区的新生代辉绿岩岩墙群、玄武岩喷发特征、盆地和地堑构造以及玄武岩中橄榄岩包体的流变学特征和断面擦痕应力场。
Many Precambrian faults and fractures have been affected by diabase dykes, which may form swarms. 许多前寒武纪断裂受到辉绿岩墙的影响,这些岩墙可以构成岩墙群。
The leachable fluorine in diabase is in direct proportion to its fluorine concentration. 辉绿岩中氟的可淋失比例与原岩中氟含量存在正相关关系。
Neoproterozoic diabase and basalt outcrop in south of Tarim Plate ( in north belt of Western Kunlun). 塔里木西南缘(西昆仑北带)发育新元古代辉绿岩及玄武岩,辉绿岩侵入青白口系而被南华系超覆,玄武岩发育在南华系下部。
At last, the concept of metamorphic pore is advanced, which can be used to interpret the cause of pore development at the external contact metamorphic belt of diabase well. 由此提出了变成孔隙的概念,较好地解释了该区辉绿岩外接触变质带孔隙发育的原因。
There are four layers of diabase in the north slope of GY sag. 高邮凹陷北斜坡第三系地层内发育了4套辉绿岩。
Distribution and Formation of Diabase Reservoir in Central Uplift of Huimin Sag 惠民凹陷中央隆起带辉绿岩油藏的分布与形成
The high-temperature hydrothermal fluids were formed by the diabase invasion into C-P in the Tertiary. 高温热流体是由第三纪时期辉绿岩侵入上古生界,引起地层水热对流形成的。
Diabase and hydrocarbon reservoir formation on the northern slope of Gaoyou sag 高邮凹陷北斜坡辉绿岩与油气成藏
Diabase in the lower contact of intrusion rocks is difficult to form favorable reservoir. 侵入岩下部接触带辉绿岩难以形成有利储层。