crustal structure 中文意思是什麼

crustal structure 解釋
地殼構造;地殼結構
  • crustal : adj. 外殼的〈尤指地球外殼〉。
  • structure : n. 1. 構造,結構;組織;石理,石紋。2. 建造物。3. 【化學】化學結構。4. 【心理學】(直接經驗中顯現的)結構性,整體性;整體結構。adj. -d ,-less adj.
  1. Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

    不同時期生成的盆地底板,將顯示地殼構造的等級次序和造陸性質。
  2. The crustal structure of junggar orogenic belt is very complex

    摘要準噶爾造山帶地殼結構復雜,構造形態多樣。
  3. In the light of the special chanacteristics of china ' s geologic structure, li siguang applied the method of geomechanics to study the law of crustal movement

    有鑒於我國地質結構的特點,李四光運用地質力學的方法,來研究地殼運動的規律。
  4. To calculate this boundary parameter, mohorovicic discontinuity palaeo - heat flow value during basin evolution process is identified through geotectonic background analogy method based on " peeling " method model, and the basin basement palaeo - heat flow is calculated through inversion from today to antiquity with current tectonic structure as constraint condition for palaeo - crustal architecture analogy

    為了求取這個邊界參數,以「剝層」法模型為基礎,通過大地構造背景類比法確定盆地演化過程中莫霍面古熱流值,以現今地殼結構為約束條件類比古地殼結構,從今至古反演求取了盆地基底的古熱流。
  5. The natural factors of the ground subsidence include crustal movement, geological structure, geology, physiognomy, and hydrology, etc. the human factor includes excessive exploitations of fluid resources, such as groundwater, etc. in the sixth part, the collection and management of data, the establishment and management of the database, and the protraction and usage of related maps in the research of ground subsidence were introduced and discussed

    地面沉降影響因素包括地殼運動、地質構造、地貌、氣候和水文等自然因素,以及過量開采地下水等人為因素。第六部分從數據的收集、整理、數據庫的建立和管理及有關圖件的繪制及應用等方面對gis在地面沉降研究應用作了介紹和探討。
  6. The control of the deep - seated structural - magmatic process over the metallogenic system around the middle - lower yangtze river reaches is shown as : ( 1 ) the mantle uplift belt is closely related to the general geological background of the metallogenic system ; ( 2 ) the primitive magma originated from different parts of the mantle uplift belt ( mantle ridge or mantle slope ) shows differences in style of formation and composition and results in different magmatic series and metallogenic subzones, respectively ; ( 3 ) the varying depths of structural - magmatic chambers may form a " three - layered structure " ( central type, network - like and ring - like ) and this is the primary factor that controls the different magmatic series and the concerned cluster of ore deposits ; ( 4 ) the alkaline basaltic magma derived from the mantle ridge forms high - potassium and calcium alkaline magma and shoshonitic magma due to its altering intensity of afc process with the lower crustal material, which has something to do with the copper - gold and iron - sulphur metallogenic subsystems, respectively

    深部構造巖漿作用對長江中下游成礦帶安徽沿江地區成礦系統的控製表現為: ( 1 )地幔隆起帶與成礦系統的總體地質背景的演變密切相關; ( 2 )源於地幔隆起帶不同部位(幔脊與幔坡)的原始巖漿,其生成方式和物質組成不盡相同,它們分別產生相應的不同巖漿巖系列和成礦亞帶; ( 3 )不同深度的構造巖漿房組成中心式網格式環帶式「三層結構」 ,是控制區內不同巖漿巖系列及有關礦床集中分佈的主要因素; ( 4 )源於地幔隆起帶脊部的堿性玄武巖漿,由於與下地殼物質發生的afc作用強度不同,形成了高鉀鈣堿性巖漿和橄欖安粗巖漿,分別與銅、金成礦亞系統和鐵、硫成礦亞系統有關。
  7. Crustal electric structure of haiyuan arcuate tectonic region in the northeastern margin of qinghai - xizang plateau, china

    青藏高原東北緣海原弧形構造區地殼電性結構探測研究
  8. Based on the comparative study of yingen - ejinaqi basin and erlian basin from the aspects of mesozoic strata, regional structures, magmatic activity, source rocks, reservoir, oil and gas reservoir formation characteristics, oil and gas distribution, and deep crustal structure, it shows that these two basins are similar to each other in regional geology amid petroleum geological features

    摘要通過對銀根額濟納旗盆地與二連盆地的中生代地層、區域地質構造、巖漿活動、烴源巖、儲層、油氣成藏特徵、油氣分佈規律及深部地殼構造等的研究,表明兩盆地的區域地質及石油地質特徵具有相似性。
  9. Wang xiaoqing and ma zongjin, 1990, deep crustal structure of north china seismic region, revealed by earthquake statistics and geopgysics data ( abstract ), international workshop on continental seismogenetic layer, april 27 - 30, beijing, china

    王曉青, 1992 ,華北地震區地震空間分佈與震源層構造特徵,大陸多震層研究,北京:地震出版社。
  10. Using various geophysical and seismogeological data available, the present paper has probed into relationship of characteristics of gravity and magnetic field, crustal structure and active faults to earthquake and summed up spatial distribution of epicenters in crustal media

    摘要本文利用現有各種地球物理資料、地震地質資料,探討了重磁場特徵、地殼結構、活動斷裂與地震的關系,進而總結出地震震中在地殼介質中的空間分佈規律。
  11. Based on abroad consultations and studies on national and foreign related datum, mainly taking shenzhen luohu fracture zone for research object, and by means of analysis on locale monitoring datum analysis, laboratory routine rheopectic testing, finite element numerical simulation and appraisal of gis stability, a few of conclusions can be summarized as the following : ( 1 ) analyzing present and past geological reconnaissance datum and reports of stability appraisal in luohu jiancheng district and synthesizing a mass of crustal stress monitoring datum and huangbeiling faultage f8 monitoring datum, and combining closely with practical engineering activity in luohu district, characteristics of crustal stress distribution is deeply discussed, which has an important guiding meaning for studying region stability and underground structure safety in luohu district

    本文在廣泛查閱、研究國內外有關資料的基礎上,主要以深圳羅湖破碎帶為研究對象,通過現場實際監測資料分析、室內常規流變試驗、有限元數值模擬以及基於gis的穩定性評價,可以得到以下幾點結論: ( 1 )分析了羅湖建成區以前和現今的地質勘察資料、穩定性評價報告,綜合大量的現今地應力監測資料和黃貝嶺f8斷層監測資料,緊密結合羅湖建成區的實際工程活動,深入探討了羅湖區的地應力分佈特徵,這對于研究羅湖地區區域穩定性和地下建築物的安全性具有重要的指導意義。
  12. After transient state process ( earthquake, etc ) having occurred, present - day crustal movement ( the changing process with time, the space distribution and the structure of spectrum ) will return to " stable steady state ( dynamic balancing state ) " voluntarily

    在地震等暫態過程發生后,現今地殼運動(時變過程、空間分佈、頻譜結構)仍將自動回歸到「穩定態(動平衡態) 」 。
  13. Study on the gravity field and deep - seated crustal structure at the altun mts - the qilian mts area

    青藏高原北緣重力場特徵與深部地殼構造
  14. Since in most rock samples poisson ' s ratio is very markedly anisotropic, some even greater than 30 % when the effect of microcracks is eliminated, the anisotopy of poisson ' s ratio must be considered when using poisson ' s ratio to inverse the crustal structure

    由於泊松比也表現出很強的各向異性,在排除微裂隙的影響後有的仍可以達到30 %以上,在利用實際地震波傳播數據通過泊松比反演地下物質結構時必須考慮其各向異性的影響。
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