- 更多网络例句与变辉绿岩相关的网络例句 [注：此内容来源于网络，仅供参考]
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The investigation indicates that the Shalagang antimony has osculatingrelationship with the Structure but has no selectivity with the host rock: The ore bodyis controlled by the fault zone, which insert into it as a nervation;The host rockincludes chert, carbonaceous slaty rock, altered diorite , altered diabase and so on. Theore-forming epoch of Shalagang antimony is obviously later than era of the host rock,so it is concluded that the Shalagang antimony maybe formed in the late Himalayan.
研究表明，沙拉岗锑矿床与构造关系密切，而对容矿岩石类型无选择性：矿体主要受控于断裂及层间破碎带；主要容矿岩石有硅质岩、碳质板岩、强蚀变中基性火山岩和蚀变辉绿岩等，并以硅质岩为主；矿床成矿时代明显滞后于容矿岩石时代，据此推断沙拉岗锑矿床可能形成于喜山晚期。
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337 Uranium ore deposit lies to the east of the Xiazhuang orefield,and there are structural fracture groups with EW,NNE-trending,diabase and syenite vein with NW-trending in the deposit region.
337铀矿床位于下庄矿田东缘，区内发育近EW向、NNE向构造裂隙群及NW向辉绿岩和正长岩脉体，发育以碱性为主的多种围岩蚀变。
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Hypogene high thermal or deep source epi-mesothermal condition and it is not only stressed the mantle source simply but also the crust-mantle;②in order to guid ore exploration better the artificial classification of uranium deposits should be broken and uranium ore-forming system strengthened;③much attention should be paid to searching the diabase-hosted rich uranium ore in strongly argillized cataclastic zone;④attention should be paid to the influence of basement of volcanic basin on the uranium ore formation that should be undstood both in feeling and theoretically through the ore propect process;⑤relation of red basin with uranium ore formation can be made clear from analyzing tectonics, paleo-climate and time and it is not only theoretically important but also helpful to uranium ore prediction;⑥crypto explosive pipe is an uranium ore, rich uranium ore host structure and it is the next goal for uranium ore exploration in east China.
摘要文章论述了华东火山岩型铀矿找矿值得重视的地质问题：①铀成矿既可形成于浅源浅成低温条件，也可形成于深源深成高温或深源浅成中低温条件，在强调深源时，不是简单地认为是幔源就可以了，还必须强调壳幔作用的地质过程；②打破人为的&类型&划分，加强&铀成矿系统&的研究，更好地指导找矿；③研究基性脉体与铀成矿问题应注意构造、岩石矿物成分、成因、蚀变与成矿3大问题，注意寻找泥岩化作用强烈的破碎辉绿岩脉中的富铀矿；④火山盆地基底对铀成矿的作用主要是提供铀源，将基底对铀成矿的影响从感性认识推向理性认识，有效地指导找矿；⑤红盆与铀成矿关系可以从构造、古气候及时间分析研究中得出结论，它不仅仅是一个理论问题，而且有助于铀成矿预测；⑥隐爆角砾岩筒是铀成矿、成富矿的重要储矿构造，是华东火山岩型铀矿找矿的新领域。
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We think main metamorphic rock types of this area include mited granite ,mixed metamorphic rock,leptite,etc.
认为变质岩中混合花岗岩、混合岩化变质岩、变粒岩、浅粒岩、黑云斜长片麻岩等为本区的主要变质岩类型；沉积岩以云岩、硅质岩和石英砂岩为主；火成岩脉主要为辉绿岩、煌斑岩和闪长玢岩。
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The low homogenization temperatures indicate that the petroleum is encapsulated at the cooling stage of the diabases that have intruded in the Es3 strata when the interaction between ground water and the feldspars resulted in alteration.
测得其中部分粒径较大的石油包裹体的均一温度 th=79～ 82 ℃，表明这些石油包裹体是辉绿岩体侵入 Es3地层冷却以后受地层水作用在发生的多种蚀变反应的过程中长石的节理、裂隙愈合带封存了渗入的烃类物质而形成的。
- 更多网络解释与变辉绿岩相关的网络解释 [注：此内容来源于网络，仅供参考]
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blastophitic：变余辉绿岩的
blastomylonite 变余糜陵岩 | blastophitic 变余辉绿岩的 | blastophitic structure 变余辉绿状结构
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blastophitic structure：变余辉绿状结构
blastophitic 变余辉绿岩的 | blastophitic structure 变余辉绿状结构 | blastoporphyric 变
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epididymite：斜板晶石
epidiabase 变辉绿岩 | epididymite 斜板晶石 | epidiorite 变闪长岩
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epididymite：斜方板晶石
变辉绿岩 epidiabase | 斜方板晶石 epididymite | 变闪长岩 epidiorite
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holyokeite：钠长辉绿岩
holtonite 小藤石 | holyokeite 钠长辉绿岩 | homeoblastic 等粒变晶状的
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metabasite：变基性岩
变辉绿岩 metadiabase | 变基性岩 metabasite | 变晶;蓓晶 blast
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metadiabase：变辉绿岩
变辉绿岩 epidiabase | 变辉绿岩 metadiabase | 变基性岩 metabasite
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metadiabase：伪辉绿岩;变辉绿岩
变晶包体 metacrystal inclusion | 伪辉绿岩;变辉绿岩 metadiabase | 伪闪长岩;变闪长岩 metadiorite
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metadiorite：伪闪长岩;变闪长岩
变晶包体 metacrystal inclusion | 伪辉绿岩;变辉绿岩 metadiabase | 伪闪长岩;变闪长岩 metadiorite
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vintlite：基长闪斑辉绿岩;温脱岩
基变凝炭岩 schalstein | 基长闪斑辉绿岩;温脱岩 vintlite | 基础 foundation