玄武岩质的

基本解释 (translations)

trappean

与玄武岩质的相关的网络例句 [注：此内容来源于网络，仅供参考]

All indications are that it is everywhere basaltic and relatively constant in composition.

所有的迹象只表明海洋地壳处都是玄武岩质的，组成也比较稳定。

Tuyon volcanic rocks are classified as alkali series, which are low in silicon, enrichedin alkali, especially enriched in kalium. The types of the volcanic rocks include trachybasalt,basanite, basalt,and phonolitic basalt.

托云火山岩具贫硅富碱，特别是富钾的特点，属于碱性系列，岩石的类型包括粗面玄武岩、碧玄岩、玄武岩、响岩质玄武岩。

The sharp difference suggests that they have different origins: the former comes from allochthonous sapropel-type organisms of the lower strata and is the remains of crude oil, and the latter is autochthonous humic-type organic matter of sedimentary rocks between the basalt layers.

玄武岩中铜矿石沥青的δ13CV-PDB为-27.3‰～-33.2‰，平均-31.97‰，沉积岩中铜矿石碳质的δ13Cv-PDB为-20.2‰～-23.2‰，平均-22.11‰，表明二者无明显成因联系，前者属腐泥型，为石油的遗迹，来自下部地层；后者为腐植型，来自原地沉积的陆生高等植物。

Kinetic equation in the baking process of purifying aphanitic graphite were researched.

讨论了玄武岩纤维的性能以及我国玄武岩纤维生产技术存在的一些主要问题。4。研究了隐晶质石墨的提纯工艺中焙烧动力学方程。

According to cpx-melt equilibrium pressure, the xenoliths types and simulating calculating of host rock REE partition pattern, source of sodic basalts is garnet lherzolite mantle, and the source of potassic basalt is metasomatic fluid altered phlogopite-containing garnet lherzolite mantle. For the alkaline basalts to sub-alkaline basalts, the melting degrees of the source rocks are 4%～15%.

根据单斜辉石—熔体平衡压力计算、所携带的包体类型及玄武岩稀土元素配分曲线的非实比部分熔融定量模拟表明，钠质玄武岩的来源为石榴石二辉橄榄岩源区，五大连池钾质玄武岩的源区是被交代的含金云母石榴石二辉橄榄岩源区，研究区碱性玄武岩到亚碱性玄武岩是石榴石二辉橄榄岩源区经4％～15％部分熔融程度的产物。

There are two evolutional trends for sodic basalts: alkaline basalt to sub-alkaline basalt and to the contrary. The fact that alkaline basalt has the higher concentration of incompatible elements and the sub-alkaline lower indicates the increasing degree of the partial melting in the mantle sources. The variety of Sr, Nd isotope compositions in different types of rocks shows their different mantle sources.

钠质玄武岩存在着碱性玄武岩到亚碱性玄武岩和亚碱性玄武岩到碱性玄武岩的变化序列；碱性玄武岩到亚碱性玄武岩不相容元素丰度逐渐降低，表明为部分熔融程度逐渐增高的产物；Sr、Nd同位素组成与岩性之间的相关性表明，各种岩浆是不同地幔源区部分熔融的产物。

According to their mineral assemblages, the granulite xenoliths entrained by Cenozoic Hannuoba basalts are divided into four groups: felsic granulites, noritic granulites, two-pyroxene two-feldspar granulites and two-pyroxene granulites, with the two-pyroxene granulites most common.

根据矿物组合特征，汉诺坝玄武岩中的麻粒岩捕掳体可划分为四种类型：长英质麻粒岩、苏长质麻粒岩、二辉二长麻粒岩和二辉麻粒岩，其中以二辉麻粒岩最为常见。

All of the above characteristics as well as poorcrystallized, abundant peridotite inclusions, few xenocrysts, and elements covariation trend indicate that the Tianheyong basalts were solidified from primitive basaltic magma.

上述所有特征以及岩石结晶程度低、富含橄榄岩包体和少量捕虏晶、元素变异关系等均表明，天和永玄武岩是原生玄武岩质岩浆固结的产物。

Distribution scope of the Emeishan basalt is quite broad, and the most main rock type is low-Ti basalts and high-Ti basalts, and has the few picritic basalts, picrites and meymechites.

峨眉山玄武岩分布范围比较广，最主要的岩石类型是低钛玄武岩和高钛玄武岩，并有少量的苦橄质玄武岩、苦橄岩和麦美奇岩。

Organic matter, pH, cation exchange capacity and contents of potassium, sodium, magnesium, copper, zinc, manganese, cobalt, iron, selenium, iodin and fluorin were determined of rock and soil samples from six main geological background areas within the main ruminant production base, in Yunnan Province, China. Results showed: 1 the red earth area of Paleozoic basalt and red earth area of carbonate the highest; the yellow-red earth area of mixture of carbonate, clasolite and basalt follows, except for its content of Co, which is relatively lower; and the purple earth area of Mesozoic clasolite, the yellow-red earth area of clasolite and the dark red earth area of Precambrian metamorphite are the lowest

对云南省反刍动物生产基地所属的6个主要地质背景区的土壤和岩石样品的K、Na、Mg、Cu、Zn、Mn、Co、Fe、Se、I和F元素及土壤的有机质、阳离子交换量和pH进行测定分析，结果表明：晚古生代玄武岩红壤区和碳酸岩盐红壤区土壤各种矿质元素都比较高，有机质含量与CEC都较高，特别是Ⅴ区最为显著；碳酸岩盐、碎屑岩和玄武岩混合型黄红壤区除了Co含量较低外，其他元素含量都居中等或偏上水平，有机质含量与CEC仅次于第1类背景区；碎屑岩紫色土区、变质岩赤红壤区和碎屑岩黄红壤区大多数矿质养分相对都比较低，有机质含量与CEC最低。

与玄武岩质的相关的网络解释 [注：此内容来源于网络，仅供参考]

aplite：细晶岩

粗玄岩本标准叫粒玄岩,是玄武岩的一种,矿物细 晶岩 ( aplite)是细晶质的浅色脉岩,以具细晶结构为特征. 细晶岩的主要矿物成分通常在花岗岩色矿物极少,偶见黑云母、角闪石,有时有少量白云母. 细晶岩与霏细岩(felsite)易混淆,

basalt：玄武岩 玄武岩

玄武岩 玄武岩(basalt)基性喷出岩的一种. 成分相当于辉长岩. 灰黑色. 常具气孔状、杏仁状构造和斑状结构. 斑晶为橄榄石、辉石、基性长石等;基质一般为细粒或隐晶质. 按次要矿物的不同,可划分为橄榄玄武岩、紫苏辉石玄武岩等;按结构构造,

dolerite：粗玄岩

辉石为b) 在我 国辉绿岩与粗玄岩(dolerite)不是同义语. 粗玄岩本标准叫粒玄岩,是玄武岩的一种,矿物细 晶岩 ( aplite)是细晶质的浅色脉岩,以具细晶结构为特征. 细晶岩的主要矿物成分通常在花岗岩色矿物极少,偶见黑云母、角闪石,

Hyaline：玻璃质的

hurricane 飓风 | hyaline 玻璃质的 | hyalobasalt 玻质玄武岩

hydrothermal solution：热液

促使岩石换质的是摄氏几百度的热液(hydrothermal solution),这个温度范围内的热液对金属之富集有很大的影响. 曾有实验证明,将玄武岩置於加热到200℃的海水中,经过200天的作用后,海水中的镁及硫酸盐会减少,而增加了钙、钾、铁、锰、镍、铜及氢等.

tholeiite：硅质玄武岩

依据地质学者的研究,澎湖群岛中,除了花屿的形成是早於距今60至65百万年前(中生代侏儸纪到白垩纪),并由安山岩质熔岩、碎屑岩及其他岩质的岩脉组成的以外,其他各岛屿主要是由距今17至8百万年前(新生代第三纪中新世)的矽质玄武岩(Tholeiite)和碱性玄武岩(Alkali Basalt),

aphanitic basalt：隐晶玄武岩;非显晶玄武岩

"aphanitic","微晶质;隐晶质;非显晶质;非显晶的" | "aphanitic basalt","隐晶玄武岩;非显晶玄武岩" | "Aphelaspis","原头虫"

hyalobasalt：玻质玄武岩

hyaline 玻璃质的 | hyalobasalt 玻质玄武岩 | hybrid coding 混合编码

hyalocrystalline：玻晶质的

hyalobasalt 玻质玄武岩 | hyalocrystalline 玻晶质的 | hyaloophitic 玻质辉绿岩的

vuggy：晶洞的,多孔的

volcano 火山 | vuggy 晶洞的,多孔的 | wacke 瓦克岩,玄武质砂岩; 玄武岩风化