查询词典 tectonic

Based on manifold materials of geophysical fetid, regional tectonics, surface activefaults, seismic activities and so on, we differentiated the seismotectonic belts in Chinamainland, and meanwhile, analyzed their active features and seismogenic tectonic conditions.

本文依据深部地球物理场、区域大地构造、地表活动断裂、地震活动等，划分了中国大陆的地震构造带，同时分析了地震构造带的活动特征和孕震构造条件。

Luzong area ; shoshonite series ; geochemistry ; rare earth element ; tectonic setting

庐枞地区；火山岩；地球化学；稀土元素；构造背景

After the collage of North China and Sibiric slab at palaeozic later period, Yanbian region is involved in the pacific tectonic province.

晚古生代华北板块和西伯利亚板块的南北向拼合之后，延边地区的区域构造背景进入了太平洋构造域。

From the fields of regional crust-mantle structure, metallogentic settings, history of tectonic-magmatic activity, distribution of high antimony anomaly, characteristics of deposit, origin of ore-forming materials (including Sb, C, Si, S, solution and associated elements), black dikes, the relation of deposit and mantle metasomatism fluid is expounded by means of geology and geophysics. Xikuangshan antimony deposit is proved to be a typical vein deposit formed by mantle metasomatism fluid. On the basis of this knowledge, the prospecting criteria of blind orebody of the deposit are given as follows: extensive structuer which indicating the activities of mantle metasomatism fluid, change of host rocks (especially exsisting shale barrier bed), silication and carbonization alteration.

文中对地幔交代流体组成、性质、活动特点及其成岩、成矿作用作了综述与探讨；从锡矿山区域壳幔结构和成矿背景、地质构造-岩浆活动史、高锑地球化学场结构分析、矿床特征、成矿物质(包括Sb、C、Si、S、流体及伴生元素)、与成矿有时空联系的暗色脉岩等方面入手，利用地质、地球物理、地球化学手段多方面论述了矿床与地幔交代流体活动的关系，论证了锡矿山超大型锑矿的地幔交代流体成因，并以此为基础提出盲矿体地质找矿标志：即指示地幔交代流体活动的构造，尤其是具有成矿元素和碱质异常、热液蚀变的断裂构造；有利的岩石物理化学性质；硅化、碳酸盐化围岩蚀变等。

The rock mass in the slote is composed of two grades, which have been forced by tectonic stress four times.

由岩性、地貌，地质力学的调查和分析，求得当地岩体曾受四次构造应力作用，边坡岩体分上、下两级。

Based on thorough study on the east part of Eastern Kunlun Orogenic belt, a valuable try by using tectonic facies to analyze non- Smithian strata are took.

通过对东昆仑东段造山带细致解剖，对运用大地构造相方法剖析混杂岩带非史密斯地层方面进行了有益尝试。

Like other branches of stratigraphy (evento-, geneto-, econo-, tectono- and sequence stratigraphy, and so on) appeared successively in recent twenty years, non- Smithian stratigraphy is aimed to deeply demonstrate the characteristics of various melanges in the orogenic belt from four-dimension splitting-converging of tectonic slices.

但仅据岩层任一性质和属性划分的地层位置不一定与其它的任一种性质或属性划分的地层位置一致，其界线往往互相交叉。

This project for 53 dwellings between party walls can be described through its tectonic (Roca Port Aventura in the stereotomic plinth of the two first floors of housing, plus buildings that, resting on the former, are rounded off with canvas roofs with silkscreen-printed tiles), or through its virtues of "non-extrusion" and "non-metaphor".

该建筑内部53套住房（罗卡湾岩溶坑立体方形底座为建筑的第一层，其上构建住宅，周围用帆布连同丝网装饰的瓷砖作屋顶），其优点在于引用&非突出&和&非象征&的表现手法。

The geological and geophysical data show that in the lower crust of young continental tectonic units may occur pervasive, non-seismic, subhorizontal and ductile flow related to thermal softening. The laminar flow drives fault-block movement of the upper crust, results in the formation of orogenic belts and sedimentary basins, and causes coupling between ductile lower crust and brittle upper crust/mantle.

大量的地质和地球物理资料表明，年轻的大陆构造活动区的下地壳可能因热软化而出现透入性非地震式顺层韧性流动，这种下地壳层流作用驱动大陆上地壳发生地震式脆性断块运动，形成盆山格局，发生圈层耦合。

The Es formation was divided into seven third order sequences based on the seismic, drilling and logging data, and plans deposition system plane distribution maps of different time were plotted by dominance phase principle. The lower Es4 is flood-overlake facies mainly; the upper Es4 is meandering stream and braided river delta deposition above the shore shallow lake background; in the Es3 period, the south mainly developed braided river, meandering stream delta, the northeast area main developed meandering stream delta, the middle area mainly developed semi-deep lakean d deep lake sediments. From lower Es3 to upper Es3, the delta scale gradually increased and the depositional area gradually moved to the east and the southeast; the Es2 period was dominated by shore-shallow lake sediments and widely developed braided river delta and delta deposits; the Es1 period was dominated by shore-shallow lake shoal deposits, and in the south developed meandering stream and braided river delta deposits.The lothological traps of the Shahejie group are mainly fluxoturbidite and stratum lateral pinch-out, and its formation and the distribution of the lothological trap were controlled mainly by the basin structure characteristic, palaeogeomorphology and tectonic activity and so on. It had a beneficial geological condition to develope sublacustrine slump turbidite fans in Jishan, Jiangjiadian and Wawu.

利用地震、钻井、测井等资料，将古近系沙河街组划分出7个三级层序，通过剖面沉积学分析，以优势相原则绘制不同时期各亚段沉积体系平面分布图：沙四下总体以洪水-漫湖沉积为特征，沙四上沉积时期是在滨浅湖背景之上发育了曲流河三角洲和辫状河三角洲沉积；沙三段沉积时期南部主要发育辫状河、曲流河三角洲，西北部地区发育曲流河三角洲，中部地区主要为深湖—半深湖沉积；由沙三下至沙三上，西北部三角洲规模逐渐增大，沉积范围逐渐向东、东南方向推进；沙二段沉积时期为滨浅湖沉积，在背景之上广泛发育了辫状河三角洲和三角洲沉积；沙一段以滨浅湖滩坝沉积为特征，南部发育了曲流河三角洲和辫状河三角洲沉积；沉积地层中的岩性圈闭以滑塌浊积岩岩性圈闭和地层侧向尖灭型岩性圈闭为主，其形成和分布主要受盆地结构、沉积古地貌和构造活动强度等因素控制，北部基山、南部江家店和瓦屋具有发育滑塌浊积扇的良好地质条件。

Do you know, i need you to come back

你知道吗，我需要你回来

Yang yinshu、Wang xiangsheng、Li decang,The first discovery of haemaphysalis conicinna.

1〕 杨银书，王祥生，李德昌。安徽省首次发现嗜群血蜱。