global tectonics造句
例句與造句
- New global tectonics
新全球構(gòu)造假說 - Professor jonathan aitchison , an expert on global tectonics , will conclude the lecture by speaking on " are we at risk in south china ? "
最后的一部份是由地球板塊活動專家艾赤心教授主講的處身華南地區(qū)的我們會否受到海嘯侵襲? - Professor jonathan aitchison , an expert on global tectonics , will conclude the lecture by speaking on " are we at risk in south china ? "
最后的一部份是由地球板塊活動專家艾赤心教授主講的處身華南地區(qū)的我們會否受到海嘯侵襲? - Professor jonathan aitchison , an expert on global tectonics , will conclude the lecture by speaking on " are we at risk in south china ? "
最后的一部份是由地球板塊活動專家艾赤心教授主講的處身華南地區(qū)的我們會否受到海嘯侵襲? 。 - Based on the analysis of the data on global metallogeny in the framework of geodynamics and study of the processes of continental evolution and metalloeny of of sanjiang , qinling and xingan - mongolia orogenic belts , we have reconsidered the geodynamic evlution and metallogeny during indosinian to early - yanshan movement in china , and established large - scale metallogenic model on intracontinental evolution we in orogenic belts . the main results are summarized as follow . ( 1 ) systematically gathering the data about large - scale and superlarge - scale deposits in the world and drawing up the map of global tectonics and metallogeny ; finding out the segmentation of circle - pacific ocean metallogenic belt and informing that the giant deposit clusters are the prominent feature of global metallogeny
本文在總結(jié)全球大規(guī)模成礦的地球動力學(xué)背景資料基礎(chǔ)上,通過深入解剖和系統(tǒng)對比我國三江造山帶南段、東秦嶺造山帶和興蒙造山帶中南部等典型造山帶關(guān)鍵地區(qū)以陸內(nèi)演化過程為核心的地球動力學(xué)演化歷史及其成礦特征,重新認(rèn)識了我國大陸印支?早燕山期的動力學(xué)演化過程及其成礦效應(yīng),建立了關(guān)于造山帶陸內(nèi)演化階段主要過程中的大規(guī)模成礦模式。 - It's difficult to find global tectonics in a sentence. 用global tectonics造句挺難的
- Viewing from the global tectonics , the authors dynamically described the dialectical relationships between extensions and compressions in time special 4 - d , and pointed out the different tectonic deformation systems corresponding to different tectonic dynamical environments . considering the geological evolution of sichuan basin , from nine aspects , the authors proved that the tectonic dynamical environments of sichuan basin , after its formation , has experienced the early extension , middle transition and late compression environments . correspondingly , as the paper suggests , a considerable attention need to be paid to the comprehensive studies of the early extensional structures , middle inversion structures and the late compression structures of sichuan basin when analyzing its tectonics
從全球構(gòu)造著眼,動態(tài)地從時間-空間四維闡述了拉張-擠壓構(gòu)造動力學(xué)環(huán)境的辯證關(guān)系,指出了不同構(gòu)造動力學(xué)環(huán)境對應(yīng)于不同的構(gòu)造變形系統(tǒng)。結(jié)合四川盆地地質(zhì)演化歷程,從9個方面論證了四川盆地自其形成以來,構(gòu)造動力學(xué)環(huán)境曾經(jīng)歷了早期拉張中期過渡晚期擠壓的過程,相應(yīng)地在對四川盆地進行構(gòu)造分析時,要注意早期伸展構(gòu)造中期反轉(zhuǎn)構(gòu)造晚期擠壓構(gòu)造的識別和綜合研究。
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