adamellite [ædə'melait]

adamellite的基本解释

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[化] 石英二长石, 石英二长岩

与adamellite相关的网络例句 [注：此内容来源于网络，仅供参考]

Early Cretaceous granitic volcanic-intrusive complex in Xiushanlinchang of northeastern Da Hinggan Mt. consists mainly of rhyolite, rhyolite ignimbrite-trachytic dacite, trachyandesite formed in eruptive cycle stage and adamellite porphyry-geode syenogranite-graphic alkali feldspar syenogranite formed in hypabyssal invasion stage.

大兴安岭东北部秀山林场一带的早白垩世花岗质火山－侵入杂岩体由喷发旋回期的流纹岩、流纹质熔结凝灰岩－粗面英安岩、粗安岩和浅成侵入期的二长花岗斑岩－晶洞正长花岗岩－文象碱长正长花岗岩构成。

The massive sulphide, lead-zinc, iron, copper deposits of the former and the porphyry copper-molybdenum deposits of the latter are the main ore types in the region.3. The conclusions drawn through the research on the Re-Os isotopic geochronology of the Chilu Mo deposit are as follows:(1) the model age of the Chilu Mo ore deposit is 105.6Ma, closely to the 87Sr/86S isochrone age of the porphyric granite, adamellite. So they are closely correlated in the genesis, and both are the production of magmatic evolution of the late Yanshan.

Cu、Mo、Pb、Zn、Au为区内优势矿种。3、对赤路钼矿床的Re—Os同位素年代学研究得出如下结论：(1)赤路钼矿的矿化模式年龄为105.6Ma，与似斑状花岗岩、二长花岗岩等的87Sr/86Sr等时线年龄115±4Ma较接近，表明二者在成因上密切相关，同属燕山晚期岩浆演化的产物；(2)赤路钼矿床具有辉钼矿中Re、Os含量偏低，低87Sr/86Sr初始值和硫同位素组成接近陨石硫等特点，表明其为成矿物质来源于地壳深部，且为斑岩型钼矿床。

The results indicate that the main lithology of the Yeniutan granite are granodi orite and adamellite, which are low in silicium, rich in aluminium, poor in alkali and rich in B, V, Zr, Ag, Pb, Zn, Cu, W, Be etc.

结果表明，该岩体主要岩性为花岗闪长岩和二长花岗岩，岩石组分为低硅过铝偏铝贫碱质，富含B、V、Zr、Ag、Pb、Zn、Cu、W、Be等元素。

The high temperature and high pressure experiments show that the strength of rocks is very high in earthquake source (mainly granitic rocks, such as adamellite), which could sustain great different stress and accumulate huge energy. This is one of major causes for high-angle reverse fault slip and high intensity of Wenchuan earthquake.

岩石破裂-黏滑-摩擦实验表明，以二长花岗岩为代表的震源区岩石具有很高的破裂强度和摩擦强度，能够承受极大的差应力和积累巨大的能量，这是高角度逆断层能够滑动和汶川地震强度大的原因之一。

The Late Triassic adamellite masses in the Yichun-Yanshou granite zone are a series of rocks with complete texture evolution .

伊春-延寿花岗岩带上的晚三叠世二长花岗岩体是一套呈结构演化系列的岩石，岩石类型按结构可划分出一期结构、二期结构、末期结构的完整系列。

与adamellite相关的网络解释 [注：此内容来源于网络，仅供参考]

adamellite：石英二长石

adamantine drill 金刚石钻 | adamellite 石英二长石 | adamic earth 红粘土

adamellite：石英二长岩

adambulacral 侧步带板 | adamellite 石英二长岩 | adamic earth 红粘土

adamellite; normal granite：石英二长岩;石英二长石

"副步带板","adambulacral" | "石英二长岩;石英二长石","adamellite; normal granite" | "红黏土","adamic earth"