隐晶岩

基本解释 (translations)

aphanite  ·  aphanitism  ·  kryptomere  ·  cornean

与隐晶岩相关的网络例句 [注：此内容来源于网络，仅供参考]

TheJiyang depression located in paleomonsoon climate zone in the period of the sahejieformation sedimentation, the wet and hot climate made ancient lake become deeperwater, enhanced stratification, reduced primary productivity of plankton, decreasingsedimentary velocity of carbonate, increasing sedimentary velocity of clay, fortifiedreductibility on certain degree, and then would be available for development of blackshale, dark shale and oil shale; In the contrast, the cold and dry climate lead ancientlake to shallower water, subdued stratification, increaser primary productivity ofplankton, enhancive sedimentary velocity of aphanitic carbonate, decreasedsedimentary velocity of clay, and then would be available for development calciteshale, calcite laminar shale, calcite mudstone, shaly carbonate rock, even laminarcarbonate or dolomite rock.

济阳坳陷在古近系沙河街组沉积期属于古季风气候带，在湿热的气候条件下古湖水加深，分层性增强，浮游生物的古生产力降低，隐晶碳酸盐的沉淀速率变小，粘土沉积速率加快，还原性一定程度上有所加强，有利于黑页岩、油页岩和暗色泥岩的形成：而相对干冷气候下，古湖水变浅，分层性减弱，浮游生物的古生产力增高，隐晶碳酸盐的沉积速率变大，粘土的沉积速率减慢，有利于钙质页岩、钙质纹层页岩、钙质泥岩、泥灰岩甚至纹层状碳酸盐岩、灰岩的发育。

Rhyolites are a group of extrusive igneous rocks with phenocrysts (visible crystals that grew out of the molten lava) of quartz and alkali feldspar in a glassy to cryptocrystalline groundmass.

流纹岩是一组受挤压火成岩矿，包含了在玻璃基的隐晶质中的石英与碱性长石的斑晶（生在于熔岩外的可见石英晶体）。

Rhyolite is the aphanitic equivalent of granite.

流纹岩是花岗岩的隐晶质等同体。

Changhua County, Zhejiang Province, China produced a Aphanitic block, to dickite and old stone-based multi-mineral rocks.

我国浙江省昌化县所产的一种隐晶质块状的、以地开石和高龄石为主的多矿物岩。

Identifying the minerals that occur as phenocrysts in porphyries is the method often used by geologists to name handspecimens of aphanitic rocks.

地质学家常用的鉴别这种矿物质的方法是根据隐晶质岩产生的斑晶，通常命名为隐晶质岩石的 handspecimens 方法。

Within these thirdorder sequences, there are many subtidal carbonate cycles that are made up of both the mediumto thinbedded aphanitic micrites and the thinbedded marls in the transgressive and the early highstand system tracts, and many grotesque sedimentary structures are developed in the bedding planes of aphanitic micrites.

在这些三级层序的海侵体系域和早期高水位体系域中，中薄层隐晶质泥晶灰岩和灰黑色薄层泥灰岩组成若干潮下型米级旋回；而在隐晶质泥晶灰岩层面上，普遍发育各种奇形怪状的沉积构造。

Several conclusions are drawn from the study. The ore deposit mainly occurs in the lower Cambrian Shuigoukou Formation, which is situated at the limbs of Qingshixia-Yujiatai overturned multiple syncline. The ore-hosted rocks are silicalite and mudstone. The content of SiO2 is high in the rocks of V ore deposit. Silicalites are mainly aphanitic quartz and chalcedony and the barite is sedimentogenic. The correlation between V and Cr, U, Ba is good. The rare earth element distribution patterns show Ce-negative or positive anomaly, obviously Eu positive anomaly and the right dip graphics.

研究结果表明，该区钒矿主要产出于青石峡－余家台倒转复式向斜两翼下寒武统水沟口组下岩段硅质岩夹泥岩的泥岩中，矿体产状与地层产状基本一致；钒矿床中所有岩石都含有较高的SiO2，硅质岩以隐晶质石英和玉髓为主，有沉积成因重晶石；V与Cr、U、Ba相关性好；稀土元素球粒陨石标准化模式具有或正或负的Ce异常和明显的Eu正异常、向右倾的图形。

LREE depleted spinel lherzolite xenoliths are the 2%～15% partial melting residues of spinel lherzolite with 2 times REE concentration of chondrite. LREE enriched spinel lherzolite xenoliths are the prodiuct that 1% partial melting of garnet lherzolite derived melts mix in ratio of 2% with most LREE depleted spinel lherzolite.

轻稀土亏损的尖晶石二辉橄榄岩包体，是2倍球粒陨石稀土元素丰度的尖晶石二辉橄榄岩地幔经过2％～15％部分熔融后的残留体；而富集型尖晶石二辉橄榄岩包体可能为，来自深部石榴石二辉橄榄岩源区1％熔融形成的熔体以约2％的比例隐交代轻稀土元素最亏损的包体代表的幔源区后形成的。

Their characters include (1) the particular configuration of the MT structures;(2) the obvious interface with rich organic matter and pyrite between the MT ribbon cracks and the host rock;(3) the host rocks are characterized by nonstromatolitic micrite limestones with few liminites;(4) the special macroscopic fossils of algae which were simultaneously developed with the MT structures.

这些特征包括：(1)臼齿状构造特别的形态学特征，(2)由微亮晶所充填的臼齿状裂缝具有明显的边界（以富集残余有机质和黄铁矿为特点），(3)臼齿状构造的宿主岩石是不发育叠层石和纹理化构造的隐晶质泥晶灰岩，(4)与臼齿状构造常常共生的极为特别的宏观藻类化石等。

与隐晶岩相关的网络解释 [注：此内容来源于网络，仅供参考]

aphanite：隐晶岩

aphaniphyric 隐晶斑状 | aphanite 隐晶岩 | aphanitic texture 隐晶结构

aphanite：隐晶岩类

aphaniphyric 显微隐晶斑状 | aphanite 隐晶岩类 | aphanitic 隐晶质的

aphanite：隐晶岩;非显晶岩

隐晶基斑状;非显晶基斑状 felsiphyric | 隐晶岩;非显晶岩 aphanite | 隐晶岩的 kryptomerous

calc aphanite：钙质隐晶岩

calc alkaline rock 钙质 碱性岩 | calc aphanite 钙质隐晶岩 | calc spessartine 钙锰铝榴石

diabase aphanite：辉绿隐晶岩

辉绿角闪石岩 diabase amphibolite | 辉绿隐晶岩 diabase aphanite | 辉绿细晶岩 diabase aplite

aphanitic texture：隐晶结构

aphanite 隐晶岩 | aphanitic texture 隐晶结构 | aphanitic variolitic texture 隐晶球颗结构

aphanitic basalt：隐晶玄武岩

隐晶岩 aphanite | 隐晶玄武岩 aphanitic basalt | 隐晶基斑状结构 aphanophyric texture

aphanitism：非显晶岩, 隐晶岩

aphanitic | 非显晶岩的, 隐晶岩的 | aphanitism | 非显晶岩, 隐晶岩 | aphanizophyll | 蓝溪藻黄素甲阿番叶素束丝藻叶黄素

cryptomere：隐晶岩

钾锰氧矿 cryptomelane | 隐晶岩 cryptomere | 隐晶的 cryptomerous

kryptomere：隐晶岩

冰扰作用 kryoturbation | 隐晶岩 kryptomere | 隐晶岩的 kryptomerous