1、

Present Tectogenesis and Characteristics of Crustal Stress Field in Datong Basin

大同盆地现今构造活动及地壳应力场特征

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2、

Crustal stress-strain observation plays an important role in earthquake prediction and tectonic stress analysis.

地壳应力应变观测在地震预报及构造应力场分析中占据重要地位。

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3、

The seismic precursory anomaly of crustal deformation and underground water level are non-cyclic changes resulted from the mutual action of the tectonic stress of earthquake preparation and fluid force produced by rain, underground water.

地壳形变与地下水位前兆异常是在地震孕育构造应力和降雨、地下水引起的流体力共同作用下产生的非周期性变化。

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4、

The geological tectonic framework and the crustal evolution in Jiangxi Province

江西省地质构造格架及地壳演化

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5、

Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation

新疆北部及邻区地壳构造格架及其形成过程的初步探讨

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6、

Through an integrated analysis of the types of tectonic deformation and metamorphism, order of their formation, emplacement of plutons and isotopic age data, this paper discusses the regional distribution and formation ages of metamorphic rocks and their role and significance in the process of crustal evolution.

通过对构造变形与变质特征、形成序次、深成岩侵位及同位素年龄资料的综合分析,阐明变质岩的区域分布和形成时代,及其在地壳演化中的作用和意义。

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7、

Extensional tectonic model of crustal elevation in western Shandong

鲁西地壳隆升的伸展构造模式

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8、

Contemporary crustal deformation and active tectonic block model of the Sichuan-Yunnan region, china

川滇地区现代地壳运动速度场和活动块体模型研究

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9、

The analyses show that the section and profile maps of China coast tectonic deformation are consistent with the coast tectonic pattern: the northern coast is characterized by large area rise drop zones with obvious boundaries, showing effects of large scale crustal movement;

分析结果表明,中国海岸构造变形的平面和纵断面图象与海岸构造格局一致:北方海岸大面积升降区比较完整,分界明显,表现出大范围块体运动特征;

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10、

Crustal structures of blocks with different features associated with tectonic evolution process are got by processing of DSS data of different blocks within the North China rift depression basin.

通过对华北裂陷盆地内不同块体的深地震测深资料处理,得到与构造演化过程相关的、不同性质块体的地壳结构特征。

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11、

Because China has been considered to be a special tectonic unit in the global tectonic theory, its crustal and upper mantle structures are interesting to many geophysicists and geologists.

本文扼要地总结了我国对深部构造研究的进展情况。曾经在几个不同地区进行过地震测深的工作,有些地区发现地壳中存在高速或是低速的夹层。

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12、

Crustal structure and earthquake distribution of the tectonic zone in eastern Sichuan and Western Yunnan Provinces

川滇构造带及其邻区的地壳结构与地震分布

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13、

Metallogenesis and crustal evolution of the Kang-Dian tectonic zone

康滇构造带的成矿作用与地壳演化历史

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14、

The crustal and upper mantle structure of Kunlun-Chaidamu-Qinling-Dabie tectonic zone is studied by using the data available from Chinese Digital Seismographic Network.

本文利用中国数字地震台网的资料,对昆仑山柴达木盆地秦岭大别山纬向构造带的地壳及上地幔构造进行了研究。

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15、

Metamorphic tectonite is a special rock formed by deformation in ductile shear belts at different crustal levels, which has a clear meaning of structural origin.

变质构造岩是由变质变形作用形成的一种特殊类型岩石,形成于地壳不同构造层次上的韧性变形带中,具有明确的构造成因的含义。

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16、

The results show that large tectonization and strong earthquakes mainly occur on the active crustal-block boundaries.

研究指出,主要构造变形和强烈地震大都发生在活动地块边界。

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17、

Setting up some fixed stations and using some instruments ( such as water tube tiltmeter, tiltmeter, tensometer, strainmeter, etc.) to continuously monitor the crustal deformation in order to catch the short-impending precursor which can be used in earthquake prediction.

建立固定形变监测台站进行连续形变的观测(如连通管、倾斜仪、伸缩仪、应变仪等),以捕捉临震的形变前兆信息,用于震前的短临预报。

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18、

Based on the terrestrial heat flow and crustal structure data, this paper calculates the temperature and the thermal structure of lithosphere in the South China Sea.

依据南海中央海盆大地热流观测值及地壳结构资料,利用地热学方法计算了海盆及周缘壳内温度和热流分布,并得出壳幔热结构配分比例。

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19、

The crustal heat production rates of Northern Xinjiang as given in the article Characteristics of Heat Production Distribution in Northern Xinjiang were verified based on the terrestrial heat flow date of the same area.

根据新疆北部地区大地热流数据,对新疆北部地区岩石生热率分布特征一文给出的地壳生热率进行检验。

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20、

Horizontal principal stress in the upper crust of China is due to the weight of the overburden rock beds themselves, the crustal temperature field as well as the compression of the plates.

地壳上部的水平主应力是上覆岩层自重、地壳温度场和板块挤压三种作用的结果。

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