花岗岩

The Baorilajinwola riebeckite granite body, located in the eastern flank of the middle section of Daxing'an Mountains, was formed in the late stage of Early Cretaceous or later.

宝日拉锦乌拉钠闪石花岗岩岩体位于大兴安岭中段东坡，形成于早白垩世晚期或更晚些。

By itself the light can only be compared to a solid, dense, rocklike, homogeneous and changeless mass of pure awareness, free from the mental patterns of name and shape.

性光好比花岗岩般实在、坚硬、密集、均一、不变的一整块纯粹的觉知，没有丝毫由心态组成的名相。

The rocks are potassium-high (K2O=4.10%~5.27%, 4.86% on average) and alkali-rich (Na2O+ K2O=7.12%~8.24%, 7.85% on average) ones, and have an average K2O/Na2O value of 1.63, ACNK values of 0.90~1.05 (0.96 on average) and KN/A values of 0.71~0.89 (0.78 on average), thus belonging to metaluminous to weakly peraluminous granitoids of shoshonite series and K-high calc-alkaline series.

岩石高钾、富碱，K2O含量为4.10%~5.27%，平均4.86%；Na2O+K2O为712%~8.24%，平均7.85%；K2O/Na2O值平均为163；ACNK值在0.90~1.05之间，平均为0.96；KN/A在0.71~0.89之间，平均为0.78，属钾玄岩系列与高钾钙碱性系列准铝质－弱过铝质花岗岩类。

The high viscosity of sialic magma makes it difficult for such magmas to reach the surface.

花岗岩。高粘度的唾液酸岩浆使人们难以对这种岩浆到达地表。

S most eastern mountains Yiwulü Mountain from the first column of the Sinian granite rock and hilly.

最东的第一列山岭医巫闾山由震旦纪岩层和花岗岩组成的低山丘陵。

It began to transform into the active continental marginin the Late Proterozoic and by the Early Paleozoic, it began to be subducted andslipped sinistrally.

海西末期华北－西伯利亚两大板块已缝合，进入超碰撞阶段，区内花岗岩大量侵位并形成了一系列推覆构造。

This class of deposits is characterized by the abundance of iron oxide in the ores and the associated intensive regional sodic alteration. They may occur in Proterozoic intracraton or Phanerozoic continental margin volcanic arcs with nearby intrusive complex or evaporite. The spatially and temporally associated intrusive rocks are magnetite-series granitoids. Mineralization mainly occurs in second order echelon structures near the main regional structure.

该类矿床以矿石中含有大量的铁氧化物且伴有很强的区域性钠质蚀变为特征，可以产于元古代克拉通内或新生代大陆边缘岛弧环境，其周围具火成岩或含蒸发盐层，时空上与之有关的侵入岩为磁铁矿系列花岗岩，矿化主要产于近区域主断裂的羽状次级断裂中。

Highly succulent stemless clump-forming plants with gray-green leaves similar in texture to lumps of granite; South Africa.

肉质无干的块状植物，有灰绿色的叶子，结构酷似花岗岩；南非。

And 5. 4～8. 5‰, respectively. Nonequilibrium oxygen isotope fractionation between rock-forming minerals and the low H〓O content indicate that depletion in D-〓O of the A-type granites from eastern China is the result of magma degassing and subsolid interaction between meteoric water and rocks.

主要造岩矿物对氧同位素不平衡分馏和全岩低水含量特征指示中国东部A型花岗岩D-〓O亏损主要受岩浆去气作用和岩浆期后大气降水亚固态交换的制约。

Mesozoic Era granites in northwestern Fujian can be generally classified into two types: remelting type and syntectic type.

闽西北中生代花岗岩总体上可分为重熔型和同熔型两种类型。

Plunder melds and run with this jewel!

掠夺melds和运行与此宝石！

My dream is to be a crazy growing tree and extend at the edge between the city and the forest.

此刻，也许正是在通往天国的路上，我体验着这白色的晕旋。