Through studies on the crustal movement in Himalayan orogenic period, paleoclimate change, types and contribution of source bodies, the geologic characteristic of the laterite gold deposit, it is believed that neotectonic period was the main mineralizing epoch for the laterite gold deposits in southern Hunan.
通過對區(qū)內(nèi)喜馬拉雅構(gòu)造運動階段地殼運動、古氣候變化特點、礦源體類型及分布、紅土型金礦床地質(zhì)特征等方面的研究,認為該階段的新構(gòu)造運動期為湘南紅土型金礦的主成礦期。
The viewpoint includes the study of the regularity of the earthquake using the overall concept of crustal movement,the forecast of earthquake using the overall concept of earthquake forecast,the division of the active tectonic system and the study of tecto.
筆者在追憶李四光地震科學和防震減災指導思想的基礎上,提出了以系統(tǒng)整體觀指導防震應急的新論點,包括:運用地殼運動整體觀研究地震規(guī)律;應用地震預測整體觀進行地震預測;劃分活動性構(gòu)造體系,研究構(gòu)造活動性;加強綜合監(jiān)測,研究各種地震前兆和相關的自然變異的發(fā)展趨勢;圈定地震風險區(qū),制定防震應急預案等。
The analysis result shows that the crustal movement of Zhangjiakou-Bohai fault zone is the strongest in the Capital Circle region.
利用GPS資料,采用聚類分析方法分析張家口-渤海斷裂帶(簡稱張渤帶)的活動性,分析表明:張渤帶是首都圈地殼運動最強烈的斷裂帶。
Its characteristics are as following:① the east and west parts in Guanzhong region crust movement vary obviously relative to the stable plate of Eurasia.
根據(jù)2001～2004年陜西省地震局GPS測站的觀測資料,做出了陜西關中地區(qū)地殼運動速率和地殼水平應變場,結(jié)果表明:①相對于穩(wěn)定的歐亞板塊,陜西關中東西部在不同期次地殼運動差異明顯;②該區(qū)最大剪應變與面應變高值區(qū)主要分布在關中地區(qū)中部的銅川-三原-西安-咸陽一帶、華縣以及寶雞-眉縣附近,應變梯度較大,并且主要受面收縮影響,地震危險性相對較高。
Monitoring crust movement by means of GPS techniques started from the end of 1980s in China.
文中主要就中國利用GPS等空間測地資料研究地殼運動、構(gòu)造變形 ,以及用于地震預測探索方面 ,從方法技術和近年來取得的一些初步結(jié)果進行了概要性論述。
On the basis of the GPS data and the relative gravimetries in some GPS stations, observed repeatedly in 1992 and 1996 in the middle section of the Himalayas,the crust movement and its mechanism are analyzed and discussed.
基于１９９２、１９９６年兩期ＧＰＳ重復觀測資料，對喜馬拉雅中段的地殼運動及其機制作了初步分析和探討。
fixed theory and the mobilistic theory of crustal movements
地殼運動的固定論與活動論
Movements in the earth could spread the radioactive12 material.
地殼運動可能會擴散這些放射性物質(zhì)。
Correlation of crustal movement Cenozoic Era on both coasts of Taiwan Strait
臺灣海峽兩岸新生代地殼運動的對比
High-Resolution Characteristics of Recent Crustal Movement in Qinghai-Tibet Plateau
青藏高原現(xiàn)今高分辨率地殼運動特征
DIVISION OF CRUSTAL MOVEMENT OF HIMALAYAN PERIOD IN YANSHAN AREA AND ITS EXPRESSED FEATURES
燕山地區(qū)喜馬拉雅期地殼運動劃分及表現(xiàn)特征
Analysis about Crustal Movement Based on Remote Sensing Image and Understanding of Earthquake
從遙感圖像分析地殼運動兼對地震的認識
The Survey and Design of the Base Stations in Tianjin Crustal Movement Observation Network
天津地區(qū)地殼運動觀測網(wǎng)絡GPS基準站的勘選
The Research on Present-day Crustal Movement and Deformation on the Basis of Global Positioning System;
基于全球定位系統(tǒng)的現(xiàn)今地殼運動與形變研究
Study on Shandong GPS Observation Network System of Crustal Deformation and Its Data Pre-Processing;
山東地殼運動GPS觀測網(wǎng)絡及其數(shù)據(jù)預處理研究
Present-day Crustal Movement of Northeastern Margin of Tibetan Plateau Constrained by GPS Observations;
基于GPS的青藏塊體東北緣現(xiàn)今地殼運動研究
Dynamic Characteristics of the Strain Fields and Crustal Movements before the Wenchuan M_S8.0 Earthquake
汶川8.0級地震前區(qū)域地殼運動與應變場動態(tài)特征
Based on present crustal movement, the potential correlation between active crustal-block movement velocity and strong earthquake activity has been discussed.
文中還從現(xiàn)今地殼運動角度,討論了活動地塊運動速率與強地震活動水平之間的可能聯(lián)系。
STUDY ON MODERN CRUSTAL MOTION IN URUMQI AND ADJACENT AREA WITH GEODETIC DATA
用大地測量數(shù)據(jù)研究烏魯木齊及鄰近地區(qū)現(xiàn)代地殼運動
ON CHARACTERISTICS OF CRUSTAL MOVEMENT OF SHANDONG AND SURROUNDING AREAS BEFORE AND AFTER WENCHUAN M s8.0 EARTHQUAKE
汶川地震前后山東及周邊地區(qū)地殼運動特征分析
diastrophic eustatism
地殼變動海面升降運動
(geology) pertaining to the structure or movement of the earth's crust.
（地質(zhì)學）關于地殼的結(jié)構(gòu)或運動的。
Reaseach on the crustal horizontal movement of Guanzhong area based on GPS
基于GPS的關中地區(qū)地殼水平運動研究
STUDY ON PRESENT-DAY VERTICAL CRUST MOVEMENT AND SEISMIC ACTIVITY IN XINJIANG AREA
新疆地區(qū)現(xiàn)今地殼垂直運動及地震活動研究