tectonic unit造句
例句與造句
- Lithospheric tectonic units of china
中國(guó)巖石圈構(gòu)造單元 - Cords for name of petroliferous basin and inferior tectonic unit of china
中國(guó)含油氣盆地及次級(jí)構(gòu)造單元名稱代碼 - Analysis on the metallogenic geological background of tectonic units in jiangxi province
江西不同構(gòu)造單元成礦地質(zhì)背景分析 - This paper gives some general principles about the division and naming of tectonic units of beishan area
摘要北山地區(qū)構(gòu)造單元?dú)w屬歷來(lái)? ?多地質(zhì)學(xué)家所關(guān)注。 - This paper gives some general principles about the division and naming of tectonic units of beishan area
摘要北山地區(qū)構(gòu)造單元?dú)w屬歷來(lái)為眾多地質(zhì)學(xué)家所關(guān)注。 - It's difficult to find tectonic unit in a sentence. 用tectonic unit造句挺難的
- Tectonically , the tectonic units consist of the gezu - xagquka suture zone and sangxuang - nagqu - midika slab in the surveyed area
構(gòu)造方面，構(gòu)造單元表現(xiàn)為各組下秋卡結(jié)合帶和桑雄那曲麥地卡板片的構(gòu)造格局；新發(fā)現(xiàn)達(dá)仁鄉(xiāng)奪列蛇綠巖體。 - The basin and mountain systems are two basic and essential tectonic units , which are developed in the temporal and spatial evolution of the crust
盆地系統(tǒng)與造山帶系統(tǒng)是大陸構(gòu)造上最突出和最基本的構(gòu)造單元，這兩個(gè)系統(tǒng)同時(shí)存在于地殼演化過(guò)程中。 - The tectonic setting in the southeast of china controlled the palaeogeographical evolution , and depositional basins have the different characteristics due to the variation of the tectonic units
中國(guó)南方東部的大地構(gòu)造背景控制著古地理演化特征,不同構(gòu)造單元內(nèi)沉積盆地的性質(zhì)存在著顯著差別。 - With numerical modeling from this method in several tectonic units in the north part of north china , the velocity structure of reflection p wave was obtained from inversion and compared with the forward solution
本文將該方法進(jìn)行了數(shù)值模擬并應(yīng)用于華北北部的幾個(gè)不同構(gòu)造單元，反演得出了其反射p波速度結(jié)構(gòu)，并與正演結(jié)果進(jìn)行了對(duì)比。 - A glide correlation analytical method for gravity and magnetic anomaly is advanced in the paper , with some application examples given , such as estimation of the nature of the anomalous source , division of oil prospects , and delimitation of boundaries of tectonic units
摘要給出了一種重磁異?；瑒?dòng)相關(guān)分析方法，并例舉了在重磁異常源性質(zhì)判斷、油氣遠(yuǎn)景區(qū)劃分、構(gòu)造單元邊界劃分等方面的運(yùn)用實(shí)例。 - Through studying about tectonic units established , old plates rebuilded , original basins restored , texture and structure of orogenic belt , mechanism and model of orogeny , it is definded that the type of beishan orogenic belt is continent - accretion arc collosion orogenic belt
通過(guò)對(duì)造山帶構(gòu)造單元的建立、古板塊重建、原型盆地恢復(fù)、造山帶結(jié)構(gòu)、構(gòu)造特徵及造山機(jī)制和模式的研究，確定北山造山帶類型為陸增生弧碰撞造山帶。 - The structure also control the formation of large and super - large deposits , which commonly lie in the cross of different directions fractures or contacting belts of different tectonic units . 4 . as a whole , gradient belts of moho discontinuity correspond to rock bodies , the flat area correspond to basement
4 、總體上，莫霍面的陡度帶一般與巖體相對(duì)應(yīng)，莫霍面的平緩區(qū)與基底具有較好的對(duì)應(yīng)關(guān)系，大型、超大型礦床一般分布在莫霍面的陡度帶_上。 - Detailed studies of tectonic unit and mineralized pedigree in each tectonic unit and each period provided that tectonic evolution passed an evolutionary sequence from early extension - transition - late compression that correspond to mineralization - sediment and submarine eruption - exhalation mineralization - moderate to acid magma and tectonic hydrothermalism that are relevant to mantle - derived magma and volcanic activities ; the mineralized pedigree can be indicated as mantle derived - inner basin and deep source - crust source ore - forming materials
對(duì)各時(shí)期、各構(gòu)造單元的成礦譜系進(jìn)行了詳細(xì)研究，提出構(gòu)造運(yùn)動(dòng)演化從早期拉張過(guò)渡晚期擠壓的演化序列，分別對(duì)應(yīng)于以幔源巖漿和火山活動(dòng)有關(guān)的成礦作用沉積及海底噴流?噴氣成礦作用中酸性巖漿及構(gòu)造熱液成礦作用；在成礦物質(zhì)上由幔源盆內(nèi)及深源殼源的成礦譜系。 - Based on an integrated analysis of the surface geological , aeromagnetic , gravity , mt and seismic data from the area of mangnai to serteng mountains in the western qaidam basin , the authors think that the qaidam basin is sandwiched between the north kunlun block and serteng tectonic belt , including two first - order tectonic units the qaidam block and the southern margin of the qilian block and four second - order tectonic units the northern margin of the north kunlun block , qaidam basin , serteng tectonic belt and suhai lake basin in the south of the qilian block
摘要通過(guò)柴達(dá)木盆地西部茫崖賽什騰山地表地質(zhì)、航磁、重力、大地電磁測(cè)深和地震資料的綜合分析，認(rèn)為柴達(dá)木盆地夾持在昆北地塊與賽什騰構(gòu)造帶之間，其中包括柴達(dá)木地塊與祁連地塊南緣2個(gè)一級(jí)構(gòu)造單元和昆北地體北緣，柴達(dá)木盆地，賽什騰構(gòu)造帶和祁連地塊南部的蘇干湖盆地等4個(gè)二級(jí)構(gòu)造單元。 - The style of deformation in different rock mass and tectonic units is varied . according to the distinction of stratigraphic assemblage , rock type . tectonic block type and the characteristics of deformation , the whole district can be subdivided into three structure belt . namely southern and northern metamorphic fold stratigraphic system and central tectonic mixed system and multi - stage intruded magmatites
根據(jù)區(qū)內(nèi)出露的地層、巖性、構(gòu)造塊體、變形變質(zhì)作用特征，全區(qū)可分為南北兩帶的變質(zhì)褶皺地層系統(tǒng)和中帶的構(gòu)造混雜系統(tǒng)以及不同期次的巖漿侵入體。
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