lamprophyre
英
美
n. 煌斑岩
双语例句
- A New Clue for Gold Searching in Xuefeng Tectonic Area& A discovery of Au mineralized Lamprophyre in Anhua
雪峰构造区的找金新线索&安化发现煌斑岩型金矿化 - Laboratory Test on Chemical Grouting of Lamprophyre Base Rock of Jinping First Stage Hydropower Station
锦屏基础煌斑岩室内化学灌浆试验研究与探讨 - Geochemistry and Origin of Lamprophyre in the Northeast of Guangxi
桂东北煌斑岩地球化学特征及其成因研究 - Potassium& Magnesium Lamprophyre Discovered in Hunan
湖南发现钾镁煌斑岩体 - Analysis of lamprophyre insert into coal seam influence to seam deposit law
煌斑岩侵入对煤层赋存规律的影响分析 - An ore-forming model with fractional crystallization of mantle-derived magma melt-crystal difference, magma, ore-bearing magma, ore-rich magma, ore-magma pulsed inrush in turn, post-mineralization lamprophyre magma intrusion and superposition mineralization has been proposed.
并提出本矿床为幔源岩浆熔离-结晶分异，岩浆、含矿岩浆、富矿岩浆和矿浆依次脉冲式贯入成矿和成矿期后煌斑岩浆侵入破坏，并叠加成矿的矿床成因模式。 - Geochemistry and origin of Late Mesozoic lamprophyre dykes in Taihang Mountains, North China
华北太行晚中生代煌斑岩地球化学特征及成因探讨 - The last remain fluid of lamprophyre magma is similar to metallogenetic fluid in composition and precipitating sequence, showing their genetic relationship.
煌斑岩岩浆晚期残余气液与成矿流体组成相近、沉淀次序相同，表明它们可能有成因联系。 - Discovery and its significance of lamprophyre in the ZAMTANG gold mineralization zone, Northwest Sichuan
川西北壤塘金成矿带中煌斑岩的发现及其意义 - This paper studies the major elements and trace elements of altered rocks and the Au content and composition of altered minerals of Jincheng gold deposit and first studied the Fe-carbonate and the amygdale in lamprophyre in this deposit.
研究了金城金矿床蚀变岩石的常量元素和微量元素、蚀变矿物的金含量和化学组成，并首次对铁碳酸盐化及煌斑岩杏仁体的组成进行了研究。 - Study on the leaching of uraniferous lamprophyre ore
煌斑岩类型铀矿石浸出方法的研究 - 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。 - Lamprophyre is closed associated with gold mineralization in the both time and space.
在空间上与金矿密切伴生，在时间上与金矿床成穿插关系。 - Recently, progresses have been made in lamprophyre study about its classification, genesis and relationship with gold deposits.
近些年来，煌斑岩研究倍受地质学家重视，在诸如煌斑岩分类、成因及其与金矿关系等问题的研究上取得了很大的进展。 - It is introduced that the lithologic features and occurrence and intrusive geologic age of lamprophyre in Tongxin mine field, and analyzed the magma intrusive passage, and studied lamprophyre intrusive features and its influence on coal seams and coal quality.
介绍了同忻井田煌斑岩的岩性及产状、时代，分析了岩浆上升通道，研究了煌斑岩侵入特征及其对煤层、煤质的影响。 - When the down_going plate enters the mantle, gold_bearing fluids accompanied by partial_melting products will rise and react on the mantle wedge, resulting in an enriched mantle that is fertile for the generation of gold_rich lamprophyre magma.
在俯冲板块进入地幔后，含金流体和分熔产物一起上升并交代地幔楔，形成能够产生富金煌斑岩浆的富集地幔。 - Geochemistry of the Lamprophyre Dykes in the SW Margin of the Tarim Block and Their Source Region
塔里木板块西南缘钾质煌斑岩地球化学及源区特征 - Discovery and Gold Preconcentration Study of the Lamprophyre Alteration-type Gold Deposits in the Qinling Area
秦岭地区蚀变煌斑岩型金矿的发现及金的预富集研究 - The lamprophyre in the mining area control not only the overall distribution of the industrial orebodies but also their occurrences and scales, and it is an important prospecting criterion.
煌斑岩不仅控制了矿区工业矿体的总体分布，而且控制了金矿体的产状及规模，是重要的找矿标志。 - The alkali lamprophyre complex from Langao County, whose chondrite-normalized REE patterns all incline to the right and whose major elements vary regularly, has abundant incompatible elements.
岚皋碱质煌斑杂岩主量元素呈规律性演化，REE球粒陨石标准化配分型式呈强右倾型，富集不相容元素。 - The potash lamprophyre belt of west Sichuan-Yunnan is located at the transitional zone between west margin of Yangtze platform and Sanjiang fold belt.
川滇西部地区钾质煌斑岩带产于扬子板块西缘与三江褶皱带之间的过渡地带，侵位于老第三系地层。 - Geochemical Characteristics and Petrogenesis of the Early Paleozoic Alkali Lamprophyre Complex from Langao County
岚皋早古生代碱质煌斑杂岩地球化学特征及成因探讨 - Advances in Lamprophyre Study
煌斑岩及其与金矿关系研究的进展 - Lamprophyre is widely distributed in the Qinling area. Most of the lamprophyre alteration-type gold deposits are discovered in both sides of the Huixian-Chenxian basin.
秦岭地区煌斑岩广泛分布，大部分蚀变煌斑岩型金矿发现于徽成盆地南侧。 - It is concluded that the lamprophyre is not the eastern boundary of antimony mineralization in the Xikuangshan mining district and there still exists prospecting potential in the east of the lamprophyre.
煌斑岩不应是锡矿山矿区锑矿化的东部边界，其东部仍具有找矿潜力。 - There is two types of mafic dikes in Lantian uranium field. One is dark green lamprophyre, minette ( according to the IUGS recommended lamprophyre classification scheme).
蓝田铀矿区出露的基性岩脉主要为两种类型：一种是深灰绿色煌斑岩脉，按国际地科联推荐的煌斑岩分类方案属云煌岩，按Rittmann的划分标准，属于亚碱性岩系。 - The compressive stress of the first phase of post-mineralization should beNE-SW to NEE-SWW, providing a intrusion space for the lamprophyre.
成矿后第一阶段为NE-SW至NEE-SWW向挤压应力，为煌斑岩侵入提供张性空间。