- 更多网络例句与浅成的相关的网络例句 [注：此内容来源于网络，仅供参考]
-
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。
-
Since a large amount of epithermal deposits were discovered in circumpacific area in 1970s',the epithermal deposits have become a significant industrial type for hosting precious metals deposits and Cu,Pb,Zn non-ferrous metals deposits.
自20世纪70年代环太平洋地区发现大批浅成低温热液型矿床以来，浅成低温热液矿床业已成为贵金属矿床和Cu、Pb、Zn等有色金属矿床的重要工业类型。
-
Qitianling granite is a post-collisional,deep-sourced and hypabyssal,early Yanshanian high-K calc-alkaline granite complex pluton.
骑田岭花岗岩是燕山早期深源浅成的高钾钙碱性复式花岗岩岩体。
-
The comparative studies of lithogeochemistry for the volcano-intrusive complexes both from Jiulongzhang and from xiangshan reveal that the chemical compositions of the volcano intrusive complexes in the two areas are very close, and the trace element spidergrams and REE patterns basically coincide with each other. It is also shown that the two volcano-intrusive complexes have the same source features and the active continental margin tectonic settings. At the same time, it is found that, from early volcanic magma activities to later intrusive magma activities, the content of SiO2 and the Rb/Sr ratio decreased, on the contrary, the content of MgO and the ratios of K/Rb, Ba/Rb and LREE/HREE increased. It is shown that the hypabyssal or ultra-hypabyssal intrusives are not the products of the volcanic magmatic differentiation.
两地区的火山－侵入杂岩的岩石化学成分及其变化特点极为相近，微量元素蛛网图和稀土配分型式也基本一致，它们具有相似的岩浆过程和统一的活动陆缘构造背景；同时，从早期火山岩浆活动到晚期浅成－超浅成岩浆侵入活动，其w(SiO2)和w/w的值降低，而w以及w/w、w/w和w/w的值增高，晚期浅成－超浅成侵入岩与早期火山岩没有直接的分异演化关系。
-
The nonsulfide zinc deposits are divided into two types of supergene and hypogene nonsulfide zinc deposits. The former is the most common, and the latter mainly includes structural controlled metasomatic deposit and manganese-enriched jet-type layered deposit.
该类矿床通常被划分为浅成和深成两种类型，浅成锌矿床是非硫化物锌矿床最常见的类型，深成非硫化物锌矿床主要有构造控制交代矿体和富锰喷流型层状矿体。
-
Based on the study of the types and calculation of the component characteristics of the fluid inclusion in quartz, it is found that the ore-forming temperature of gold deposit is mainly at the two temperature zone: 170~220℃ and 230~300℃. The result shows that this deposit belongs to mesothermal type. The mineralization pressure is 51.12~72.6 MPa, and the mineralization depth is 1.7~2.4 km, which reflecting the mineralization characteristic of middle-shallow layer.
通过对其石英流体包裹体类型、包裹体的成分特征的研究及计算，得出金矿床成矿温度主要在170~220℃和230~300℃这两个区间，应属中温热液矿床；成矿压力为51.12~72.6MPa；成矿深度为1.7~2.4km，反映了中浅成的成矿特征。
-
Xiangshan volcano-intrusive complexes is the wall rock of the biggest volcanic-rock uranium ore deposit in China, and the main body is rhyolitic porphyroclastic lava, accompanied by hypahyssal or ultra-hypabyssal intrusive rocks such as dacite-porphyry and granite-porphyry Jiulongzhang volcano-intrusive complexes are dominantly rhyolitic welded tuff, accompanied by dacite-porphyry and quartz monzonite-porphyry, and so on, and the uranium resources are being assessed.
相山火山－侵入杂岩是华南地区最大的火山岩型铀矿赋矿围岩，其主体岩石为流纹质碎斑熔岩，浅成－超浅成侵入岩有英安斑岩、花岗斑岩等；九龙嶂火山－侵入杂岩的铀资源潜力尚待评价，主体岩石为流纹质熔结凝灰岩，浅成－超浅成侵入岩有英安斑岩、石英二长斑岩等。
-
The Xiaoxinancha copper-gold deposit occurs in the upwarped zone rimming the Mesozoic volcanic basin, being of porphyry type; the Naozhi gold deposit occurs in the lifted block within the Mesozoic volcanic basin, belonging to porphyry epithermal transitional type; the Wufeng and the Ciweigou gold deposit, which are two epithermal deposits, exist in the fault zone within the Mesozoic volcanic basin.
小西南岔金铜矿床产于中生代火山岩盆地边缘的隆起带，属于斑岩型矿床；闹枝金矿床产于中生代火山岩盆地内的断隆块，属于斑岩-浅成热液过渡型矿床；五凤和刺猬沟金矿床产于中生代火山岩盆地内断裂带，属于浅成热液型矿床。
-
The Zijinshan Copper Gold Deposit in Fujian Province is a high sulfur epithermal deposit discovered at first in China.
福建省上杭紫金山铜金矿床是我国大陆发现的首例高硫型浅成低温热液矿床，在矿床深部相继发现了斑岩型铜矿、中低温热液型铜矿和低硫浅成热液型银矿。
-
According to the ore-forming depth,epithermal Au-Ag polymetallic deposits distributed from b...
同时，根据我国浅成低温热液Au、Ag多金属矿床特征尝试性提出了浅成低温热液型银矿床的成矿规律与找矿标志。
- 更多网络解释与浅成的相关的网络解释 [注：此内容来源于网络，仅供参考]
-
HYP：双曲线的
hyp 亥普 | hyp. 双曲线的 | hypabyssal instrusive 浅成侵入体
-
supergene deposit：浅成矿床
supergene 表生的 | supergene deposit 浅成矿床 | supergene enrichment 浅生富集
-
hyomandibular cartilage：舌颈软骨
软舌螺 Hyolithes | 舌颈软骨 hyomandibular cartilage | 半深成的;浅成的 hypabyssal
-
hypabyssal：浅成的
hypabyssal浅成的 | hypautomorphiccrystal半自形晶 | hypautomorphicgranulartexture半自形粒状结构
-
hypabyssal：半深成的;浅成的
舌颈软骨 hyomandibular cartilage | 半深成的;浅成的 hypabyssal | 半深成岩;浅成岩 hypabyssal rocks
-
hypabyssal：浅成的 半深成的
hyoxemia /低氧血症/ | hypabyssal /浅成的/半深成的/ | hypaethral /露天/
-
hypabyssal instrusive：浅成侵入体
hyp. 双曲线的 | hypabyssal instrusive 浅成侵入体 | hypabyssal rock 浅成岩
-
hypabyssal rocks：半深成岩;浅成岩
半深成的;浅成的 hypabyssal | 半深成岩;浅成岩 hypabyssal rocks | 原地腐积 hypautochthony
-
hypaethral：露天
hypabyssal /浅成的/半深成的/ | hypaethral /露天/ | hypalgesia /痛觉迟钝/痛觉减退/
-
epithermal：低温热液的,浅成热液的
表层,上皮,皮膜 epithelium | 低温热液的,浅成热液的 epithermal | 低温热液矿床,浅成热液矿床 epithermal deposit