火山构造

Ⅲ级分为正向、负向火山构造；

The ⅲ grade be the positive , negative volcanic structure ;

三级火山构造直接控制着矿田（床）的成生。

The third volcanic structure controls the forming of mineral deposits directly .

不同级别、不同发展阶段的火山构造对化石沉积层的形成、分布和保存起到了不同的作用。三级火山构造控制了义县火山沉积岩系呈NE向展布；

The volcanic structures of various grades and different stages affected the formation , distribution and preservation of fossil-bearing beds in various degrees .

矿田受区域构造和火山构造联合控制。

The orefield is jointly controlled by regional and volcanic structures .

受火山构造环境影响，地震活动存在着外围边缘强，震源深度分布深；

Volcanic tectonic environment has influence on seismicity in the area .

同期叠置式火山构造地层层序的建立&以福建永泰油洋地区早白垩世寨下组火山岩地层为例

On the Establishment of the Sequence of Synchronous and Superimposed Volcano-Tectonic Strata

浅谈火山构造的分级分类体系

Preliminary Study on Grade and Classification System of Volcanic Tectonics

括苍山地区火山构造

Volcanic structure in kuocang - Shan District of Zhejiang

地震记录的频谱分析表明，该震群为典型的火山构造类型地震。

The spectrum analysis shows that the earthquakes are typically volcanic tectonic earthquakes .

福建省中新生代古火山构造基本特征

Basic characteristics of Meso-Cenozoic paleovolcanic structures in Fujian Province

燕山旋回火山构造成矿地球化学特征

Geochemical mineralization features of volcanic structures in Yanshan cycle

中心型火山构造的动力学机制

Dynamic mechanism of central type of volcano structure

在天然气水合物勘探中，海底的泥底辟和泥火山构造是重要的研究对象。

Both shallow and deep gas plays are present in the mud diapir belt .

巴家滩杂岩体位于庐枞中生代火山构造洼地的中心。

The Bajiatan complex is located at the center of the Mesozoic Lujiang-Zhongyang volcano-tectonic depression .

区域线型构造发育，与环形火山构造组合，形成火山岩区特有的线一环构造格局。

The regional line structure and ring structure form special line-ring structure in the volcanic area .

火山构造&岩浆活动形迹解释的数学地质方法探讨

A probe in mathematical geology technology to interpret the formality of volcanic structure and magmatic activity

火山构造作用引起的山地灾害斑块状分布较为明显。

By contrast , the porphyritic distribution of mountain hazards caused by volcano-tectonic activity is quite obvious .

岩体的分布明显地受北东向，北北东向区域构造和火山构造的控制。

The distribution of the bodies is obviously controlled by the NE-NNE trending regional structures and volcanic structures .

火山构造单元划有火山喷发带、火山构造带、火山机体三级。

The volcanic tectonic units are classified into volcanic eruption zone , volcanic tectonic belt and volcanic edifice .

确定火山构造类型、总体布局及其与基底构造的关系。

The types of volcanic structures , their distribution pattern and the relationship with base structure are defined .

酸性、中酸性岩区火山构造洼地岩相构造成矿（找矿）模式

Petrographic , Structural and Metallogenic Model of the Volcano-Tectonic Rent in the Acid and Intermediate Acidity Rock Terrain

反射地震方法较其他物探方法而言具有较高的分辨率，在研究火山构造等复杂构造方面具有优势。

In the study of volcanic structures and other complex structures Seismic method has advantages in terms of higher resolution .

火山构造组合研究和地质填图方法&以福建闽清测区1∶5万区域地质调查为例

On volcano-tectonic associations and their geological mapping & an example from 1 ∶ 50 000 regional geological surveying in Minqing area , Fujian

但是反射地震探测理论是基于层状模型的，对于火山构造等复杂构造存在一定的局限性。

For the seismic theory is based on horizontal layered model , the application on the volcanic structures and other complex structures has some limitations .

由多组断裂构造和火山构造交切及矿前水云母化提供的成矿通道和储矿条件；具有燕山晚期和喜山期发生的热液蚀变成矿作用的相互叠加；

The intersection of multiple sets of faulted structures with volcanic structures as well as mineralizing channel and the ore preservation conditions provided by the pre-ore hydromicazation ;

本文把抚州&绍兴地区的火山构造分类成四级：Ⅰ级为火山活动带；

In this paper , volcanic structure in the Fuzhou-Shaoxing area can be classified into ⅳ grades : the ⅰ grade be the zone of volcanic activity ;

然而，景点中有些火山构造的命名却存在着明显的错误，如：熔岩丘和增生熔岩球分别被错误地命名为“喷气锥”和“火山弹”。

Two volcanic structures , hornitos and accretionary lava ball , were wrongly named as " fumaroles " and " volcanic bomb " respectively in the Geopark .

福建德化&永泰巨型环状火山构造成因探析火山灰和火山岩在喷射口堆积构成了火山。

Explore and analyse the cause of the volcanic struction of Fujian Dehua-Yongtai huge ring volcanic structure volcanic ash and lava build the mountains that we call volcanoes .

本区调工作以遥感地质为先导，在填图中从调查单个火山构造扩展到多个、多种火山构造组合叠置关系及火山群体的研究。

By using remote sensing images , not only separate volcanic structures , but also various kinds of superimposed volcano tectonic associations and volcanic groups were observed during the mapping .

火山构造成岩－成矿作用过程中，体系与其环境之间的能量与物质交换，发生各种非线性的不可逆过程。

In the course of rock formation and mineralization of volcanic structure , exchange of energy and material between the system and its environment occurs as various non-linear irreversible processes .