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Tours 图尔 Le chteau de Saché萨榭城堡 Blois 布卢瓦 Le Chteau de Blois 布卢瓦城堡 Here, as elsewhere, lightness and grace are the keynote; and the recesses of the windows, with their happy proportions, their sculpture, and their color, are the empty frames of brilliant pictures.
这里和别处一样，轻松优雅是主调；深凹的窗户，因为其比例和谐，雕工精细，这里和别处一样，轻松优雅是主调；深凹的窗户，因为其比例和谐，雕工精细，色彩斑斓，成了一幅画面灿烂的空画框。色彩斑斓，成了一幅画面灿烂的空画框。
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By using Hasbrouck model to test the asymmetric information contained in price and its influence through the analysis of stock price and volume,we find out for the first time that market trade informationcontained in the object stocks in Shanghai and Shenzhen A-share stock markets is a dumbbell shape with both ends issymmetrical,different from
尝试采用投资者心态模型从投资者的守旧性和表征性启发式思维方式角度解释沪深A股市场惯性及反转效应异象形成的原因，并采用沪深A股市场的实际交易数据进行模拟验证。
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The characters of geochemistry are rich alkali. And at the same time the content of calcium is high. They are rich in alkali, high in Potassium, enriched in LILE, LREE and Pb, depleted in HFSE and have a small Sr, Nd, Pb isotope range. Their source is probably a kind of even metasomatic mantle. This is consistent with the fact that there is kimberlite containing flogopite in the deep-source enclosure of Cenozoic super-K alkali lava in the southern part of this rock zone.
组成这些钾质碱性岩带的岩石：在岩相上，包括深成相、浅成相和喷溢相等不同岩相；在岩性上，从超基性、基性、中性到酸性岩石；造岩矿物，从超基性到酸性岩石中均有透辉石，在基性、超基性岩中有霞石；在岩石化学成分上，所有岩石均表现出富碱高钾富钙，微量元素富集Rb、Sr、Ba等大离子亲石元素和Th、U等放射性元素，贫Nb、Ta、Zr、Hf等高场强元素；稀土元素富集轻稀土，铕负异常不明显；Sr、Nd、Pb同位素组成，显示了物质来源于富集地幔源区。
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Plutonic igneous rock having visibly crystalline texture.
深成火成岩石，有明显的晶体纹理。
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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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Combined with the regional data the research indicates that (1) the Tianmenshan main body formed in the Middle Jurassic Epoch, whereas the minor body was the further differentiated and evolutive product of the main body;(2) in the Chongyi-Dayu-Shangyou ore concentrated area, the west of Gannan area, the diagenetic age and metallogenic age are basically concordant, and the mineralization concentrated during 150~155 Ma;(3) from the middle-plutonic granite intrusion to the hypabyssal granite-porphyry vein, the magmatic activities experienced only 1~5Ma, indicating there was the concentrated period of mineralization.
结合区域资料，研究表明：①天门山岩体的主体形成于中侏罗世，补体是主体进一步分异演化的产物；②在赣南西部的崇余犹矿集区内成岩与成矿的年龄基本上是协调一致的，成矿集中期为150～155 Ma；③岩浆活动由中深成相花岗岩侵入体演化到浅成相花岗斑岩脉仅相差1～5Ma，表明存在成矿集中期。
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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。
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Capsules deeply lobed into 3 schizocarps, only 1 or 2 developed, loculicidal into 3 carpels; pericarp rigid, woody.
蒴果深裂的成3分果，只是发育的1或2，室背开裂成3心皮；果皮硬，木。
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Mineralogic characteristics of quartz of this gold deposit, such as REE, fluid inclusion, chemical composition, unit cell parameter, infrared absorption spectrum and thermoluminescent effect, were studied systematically in this article,and some valuable information of genetic and prospecting criteria are concluded.
本文较系统地研究了该金矿床石英的稀土元素、包裹体测温、化学成分、晶胞参数、红外吸收光谱及热发光效应等矿物学特征，总结出了有重要参考价值的成因信息和找矿标志。认为康古尔金矿床主要系中深成中低温热液成因，成矿物质具深源性，直接来自围岩火山岩。
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An igneous rock consisting chiefly of pyroxenes.
深成火成岩石，有明显的晶体纹理。
- 更多网络解释与深成的相关的网络解释 [注：此内容来源于网络，仅供参考]
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abysmal：深海的;深成的
abwattCGS 电磁制瓦特 | abysmal 深海的;深成的 | abysmalarea 深海区
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intratelluric：地内的;地下生成的;深成的
intrastructure 内壳构造 | intratelluric 地内的;地下生成的;深成的 | intratomic 原子内的
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plutonian：[地质]深成的
vinylpyridine 乙烯基吡啶 | plutonian [地质]深成的 | unsensational 不煽动感情的,不令人兴奋的,不追求轰动的
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plutonic：深成的
pluton of mesozone 中带深成岩体 | plutonic 深成的 | plutonic activity 深成活切
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hydroplutonic：水液深成的
hydroplutonic 水火成的 | hydroplutonic 水液深成的 | hydropolymer 氢化聚合物
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hydroplutonic：水火成的 水液深成的
hydropleuritis积水性胸膜炎 | hydroplutonic水火成的 水液深成的 | hydropneumatic水气并动 水气并用
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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
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hypabyssal：浅成的 半深成的
hyoxemia /低氧血症/ | hypabyssal /浅成的/半深成的/ | hypaethral /露天/
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hypogene：深成的;上升的
hypogeic 地下的 | hypogene 深成的;上升的 | hypogeneaction 深成作用
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hypogenic：深成的
hypogenewater 上升水 | hypogenic 深成的 | hypogenicaction 深成作用