核部

富Se岩石和缺Se岩石各自产于褶皱的两翼和向斜核部。

Se_rich rocks are located in either the flanks or synclinal core .

大别造山带核部典型燕山期花岗岩岩浆演化的p-T轨迹

P-T path of magma evolution of typical Yanshanian granites in the core of Dabie orogenic belt

秦岭造山带核部新元古代碰撞变形及其时代&强变形同碰撞花岗岩与弱变形脉体锆石SHRIMP年龄限定

Neoproterozoic Collisional Deformation in the Core of the Qinling Orogen and Its Age : Constrained by Zircon SHRIMP Dating of Strongly Deformed Syn-collisional Granites and Weakly Deformed Granitic Veins

方法：SD大鼠脑右侧基底核部注入淀粉样β蛋白（Aβ）和鹅膏氨酸。艹覃混合物以造成拟似痴呆模型。

METHODS : A mixture of β amyloid ( A β) and ibotenic acid ( IBO ) was injected directly into right basal brain ganglia of SD rats to build the simulant dementia model .

滥木厂铊矿床产于NE向滥木厂鼻状背斜核部和近核部，并严格受控于与背斜关系密切的NE向断裂组。

The Lamuchang Thallium deposit occurs in the core and near the core of the NE Lanmuchang anticline , and is controlled by NE-SW faults , which have relationship with the Lanmuchang anticline .

豫西东秦岭造山带核部杂岩中大理岩Pb-Pb等时线年龄及其地质意义

Pb-Pb dating of marbles from the core complex of East Qinling orogenic belt , western Henan and its geological implication

文章的主要目的是阐明占据造山带核部的大喜马拉雅结晶岩带（GHC）的侵位历史。

A main focus of the review is to elucidate the emplacement history of the high-grade Greater Himalayan Crystalline Complex ( GHC ) that occupies the core of the orogen .

浑圆状锆石核部SHRIMPU-Pb谐和年龄为620Ma和219Ma，这表明该石英闪长斑岩的母岩浆可能起源于经历了超高压变质作用改造的华南地块基底物质的部分熔融。

SHRIMP U-Pb concordia ages of the cores of rounded zircons are 620 and 219 Ma , suggesting that the parental magma for the quartz diorite porphyry may have been derived from partial melting of basement materials of the South China block that had been modified by ultrahigh-pressure metamorphism .

以基底为核部的推覆体打击底部，比如船的底部。

Strike the ground , as with a ship 's bottom .

背斜核部雷口坡膏盐层厚度巨大。

The anticline core has great thickness of salt layers .

核部有强力侵位的早白垩世的房山花岗闪长岩株。

The Fangshan granodiorite pluton of Lower Cretaceous occupies the middle of core .

东秦岭造山带核部杂岩水热系统演化机制

Evolution mechanism of hydrothermal system in the core complex of the eastern Qinling orogenic belt

推挽式双向电流源型高频链逆变器及其软缓冲技术以基底为核部的推覆体

Push-Pull Bi-Directional Current Mode High-Frequency Link Inverter and Its Soft Snubber Technique ; basement-cored nappe

主要载金矿物黄铁矿的生长环带中金的含量边缘比核部高，亮带比暗带高。

The content of gold in outer zones and bright belt of zonal pyrite are higher .

简单锆石和复杂锆石核部残留锆石均为变质成因；

Simple zircon and the smaller relict core in complex zircon are both of metamorphic origin .

燕子沟金矿床位于四川甘孜州丹巴县，永西穹窿核部。

Yanzigou gold deposit is located in Yongxi dome core of Ganzi Danba county in Sichuan province .

背斜褶皱的核部在断层间受到挤压，遭受到很强的破坏。

The core of the anticlinal fold , which is squeezed between faults , underwent intense crushing .

库区大型崩塌主要发生在背斜核部厚层灰岩陡崖分布地带；

The large rockfalls in the area mainly happened in the distribution zone of the thick limestone glint ;

坝基可能存在沿背斜核部、左坝肩断层破碎带集中渗漏问题及绕坝渗漏问题。

Dam foundation may exist piping and abutment leakages along the anticline core and left abutment shattered fault zone .

上述成果为核部杂岩，乃至整个造山带的地壳演化提供了新的证据。

These results lend the new evidence for the evolution of the core complex and the whale orogenic belt crust .

大别造山带核部晚中生代岩浆侵位序列与构造体制转换

Late Mesozoic Magmatic Intrusion Sequences Implication for the Transition of Tectonic Regimes , Central of the Dabie Orogenic Belt , China

这一研究表明，大别造山带核部存在晚侏罗世&早白垩世火山活动和火山盆地，也说明在这一时期，该区的构造环境与北淮阳地区相似。

It is also suggested that the tectonic environment was probably similar to that of the North Huaiyang in the north .

早&中侏罗世盆地分布于印支运动形成的向斜坳陷核部，属于压陷挠曲型盆地。

The third period during Early-Middle Jurassic was a compress-flexing basin which developed within the core of the syncline deformed by Late Indosinian movement .

Es2+3段油藏发育在核部，具有统一油水界面，为典型的构造油藏。

Es2 + 3 reservoir is a typical structural reservoir , developed in the core area with a uniform OWC ( oil-water contact ) .

黄陵背斜核部中段的石英脉型和蚀变岩型金矿，具有斜列侧伏性、群聚分带性、似等距性、自相似性及易采、易选等特点。

In the middle core of Huangling anticline , there are two types of Au deposits , quartz vein type and alteration rock type .

就像地球的核部一样。地幔也可分为两个同心圆圈层，下地幔和上地幔。

Like the core of earth , the mantle can also be divided into two concentric layers , the lower mantle and the upper mantle .

因此，进一步勘探主要应放在该古隆起核部周边及其向西和向东延伸的地区。

Therefore , further exploration will focus on the periphery , the extended parts in the west and east of the core of the palaeohigh .

相反，角闪石环带从核部到边部钛、铝和（钾+钠）含量减少，则暗示了角闪岩-麻粒岩相或角闪岩相到（亚）绿片岩相的退变质演化。

However , Ti , Al and ( K + Na ) decreasing likely indicate another retrogressive evolution from amphibolite-granulite or amphibolite to low greenschist facies .

尽管处于同一构造样式内，克拉2背斜构造核部和两翼部位的储集层物性仍表现出明显的差异。

There are strong heterogeneous characteristics of reservoir property between the core and limbs of the Kela-2 anticline , although they are in the same structure .

柯坪露头断裂相分析表明，碳酸盐岩断层核部多致密，破碎带中的裂缝带是油气输导的优势通道。

It is indicated that most of the fault cores are tight , but the fracture bands in damage zone are favorable paths of hydrocarbon migration .