tectonic belt造句
例句與造句
- Stratigraphic classification and correlation in es3 of jiuzhou - gu an tectonic belt
固安構(gòu)造帶沙三段地層劃分與對(duì)比 - The central tectonic belt is complex in strata , reflected by matching up of rock blocks with different ages x lithology and scales
中間構(gòu)造帶地層復(fù)雜，層序混亂，表現(xiàn)為不同時(shí)代、不同巖性、不同規(guī)模的構(gòu)造塊體的相互拼貼。 - Jiangda tectonic belt lies in the north of the three - rivers ( nujiang , lancangjiang , and jinshajiang ) tectonic belt , sw china ; the east of changdu massif ; the west of jinshajiang faults zone
江達(dá)構(gòu)造帶地處西南三江構(gòu)造帶北段，昌都地塊東緣，金沙江斷裂帶西側(cè)。 - Tectonic - lithogenic - mineralogenetic epoch and its geologic history evolution indicate that intracontinental rifting stage ( t3 ~ e1 ) is the main metallogenic period of the jiangda tectonic belt
構(gòu)造-成巖-成礦定年與地史演化研究表明，江達(dá)構(gòu)造帶主成礦期為陸內(nèi)裂谷期。 - The independent jiangda tectonic belt has appeared since late carboniferous , following the jinshajiang ocean crust of subducted beneath the changdu continental crust and the continental margin arc formed in east of changdu terrane
自晚石炭世金沙江洋洋殼開(kāi)始向昌都陸殼地體邊緣下俯沖，形成陸緣弧以來(lái)，獨(dú)立的江達(dá)構(gòu)造帶就得以產(chǎn)生。 - It's difficult to find tectonic belt in a sentence. 用tectonic belt造句挺難的
- The three gorge reservoir , locating at the suture between two arc tectonic belts of daba mountain and bamianshan , has strong structural deformation and versatile structural patterns
摘要通過(guò)分析大量資料并結(jié)合野外地質(zhì)工作，對(duì)三峽庫(kù)區(qū)的區(qū)域構(gòu)造背景及巴東組的主要構(gòu)造樣式進(jìn)行了總結(jié)，分析了這些地質(zhì)要素對(duì)三峽庫(kù)區(qū)變形斜坡形成和發(fā)展的影響。 - They all belong to the calc - alkaline island arc series and are closely related to the evolution of the arc - basin systems of the gangdise tectonic belt . based on studies of petrology , litho - geochemistry , tectonic setting , petrogenesis and magmatic evolution , the present dissertation summarized the general evolutionary regularity of the magmatic rocks in time and space . the magmatic rock assemblages are divided into the inter - arc spreading basin t
在對(duì)研究區(qū)主要礦產(chǎn)分布特征、成因類型系統(tǒng)分析的基礎(chǔ)上，總結(jié)了措勤地區(qū)構(gòu)造巖漿演化與成礦的關(guān)系，并將研究區(qū)成礦系統(tǒng)劃分為匯聚大陸邊緣成礦巨系統(tǒng)、碰撞造山成礦巨系統(tǒng)和陸內(nèi)匯聚成礦巨系統(tǒng)。 - 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。 - Zijingguan fault zone is the main structure in taihang mountains that are located in the central part of 20 ~ 30 ne - striking daxing ' anling - taihan - wuling tectonic belt . it is composed of two diagonalized faults that are wulonggou - shanghuangqi fault located in the west and zijingguan - lishan fault in the east
紫荊關(guān)斷裂帶是大興安嶺?太行山?武陵山構(gòu)造帶中段太行山地區(qū)的主體構(gòu)造，總體走向20 30 ，由西側(cè)的烏龍溝?上黃旗斷裂和東側(cè)的紫荊關(guān)?靈山斷裂左階斜列組成。 - Through the gee stress test of finite points and finite element back - analysis , the paper concludes the geo - stress distribution pattern in different tectonic belt and various lithology strata , which will supply references to mining , design and farther decision making
摘要通過(guò)對(duì)有限個(gè)點(diǎn)的地應(yīng)力測(cè)試，結(jié)合已知的工程地質(zhì)條件，進(jìn)行有限元反演計(jì)算，并對(duì)結(jié)果進(jìn)行分析，得到不同構(gòu)造帶應(yīng)力分布規(guī)律和不同巖性地層地應(yīng)力的變化情況，為煤層開(kāi)采設(shè)計(jì)和進(jìn)一步的決策提供重要的參考依據(jù)。 - Lying at the core part of qinling orogenic belt , the weishancheng au - ag polymetallic ore belt is a complex tectonic belt produced by repeated convergence , piecing together and welding of several strata and terrains which were formed in different tectonic settings and had their respective formation characteristics as well as independent deformation , metamorphic and tectonic evolutionary sequences
摘要圍山城金銀多金屬成礦帶處于秦嶺造山帶東段核部，其由多個(gè)形成于不同構(gòu)造環(huán)境，有著各自獨(dú)立的建造特徵、變形變質(zhì)和構(gòu)造演化序列的構(gòu)造地層地體，經(jīng)多次聚合后拼貼并焊結(jié)為一體的復(fù)雜構(gòu)造帶。 - During this evolution , seven second - order tectonic units were formed ; from north to south are the mingqianri cretaceous residual sea basin , the arsuo tectonic melange zone , the taricuo - wenbu yenshan magmatic arc belt , the cuoqin - bangduo late paleozoic composite back - arc basin , the jiangrang - geerdi faulted uplift , the gangdise - chazi himalayan magmatic arc belt , and the xigaze - anba fore - arc basin . these units comprise important parts of a poly - arc - basin system and exhibit evolutional features of mesozoic to cenozoic arc - basin systems . mosaic pattern of these tectonic units delineates the lithosphere coupling processes of the gangdise tectonic belt under mechanisms such as back - arc basin attenuation and arc - continent collision
自中新生代以來(lái)，岡底斯構(gòu)造帶經(jīng)歷了洋殼俯沖、弧陸碰撞、陸內(nèi)俯沖-碰撞、走滑和塊段隆升的多階段構(gòu)造演化歷程，形成了由北向南七個(gè)二級(jí)構(gòu)造單元，即岷千日白堊紀(jì)殘余海盆、阿索構(gòu)造混雜巖帶、它日錯(cuò)?文部燕山期巖漿弧帶、措勤?幫多晚古生代復(fù)合弧后盆地、江讓?格爾耿斷隆、岡底斯?查孜喜馬拉雅期巖漿弧帶、日喀則?安巴弧前盆地。 - This paper discusses the evolution , metallogenic law , and ore - prospecting direction about the jiangda tectonic belt , by studying tectonic evolution and tectonics - metallogeny coupling relationship , guiding by theories of terrane - plate tectonics and tectonics - metallogeny , basing on the thought that different tectonic regime has different geologic - metallogenesis , and the conversion of multiple tectonic regimes conduces certainly to the generalized homothetic composite action of multiple metallogenic subsystems , and forming the multiple - composite metallogenic system
本文以地體?板塊構(gòu)造理論和構(gòu)造成礦學(xué)理論為指導(dǎo)，通過(guò)深入研究江達(dá)構(gòu)造帶的構(gòu)造演化及構(gòu)造?成礦耦合關(guān)系，本著不同構(gòu)造體制具有不同地質(zhì)?成礦作用，多種構(gòu)造體制演繹導(dǎo)致多元(個(gè))成礦體系的廣義同位復(fù)合構(gòu)成多元復(fù)合成礦系統(tǒng)的思想，對(duì)江達(dá)構(gòu)造帶的構(gòu)造演化、成礦規(guī)律和找礦方向進(jìn)行了系統(tǒng)的研究。 - And the generalized homothetic composite action of metallogenic subsystems mentioned above formed the multiple - composite metallogenic system of the jiangda tectonic belt . the typical ore deposits of jiangda tectonic belt , such as dingqinnong , jiaduoling , renda etc , are contact metasomatic type deposits formed intracontinental rifting stage , and the tectonic - magmatic - hydrotherm of intracontinental orogenic stage superposed and rebuilt some preexistent ore body . their space distribution is controlled by composite intrusive rock belt of ne direction
對(duì)丁欽弄、加多嶺、仁達(dá)等典型礦床的研究表明，它們均為形成于陸內(nèi)裂谷作用階段的接觸交代型礦床，陸內(nèi)造山期的構(gòu)造?巖漿?熱液作用疊加改造了先成礦體，礦床空間分布受北東向復(fù)合侵入巖帶控制。 - In north of whole three rivers tectonic belt include jiangda tectonic belt , regional geochemical research indicate that its geochemical anomaly present the character of belt in nw direction and trip in ne direction , too . this is the geochemical response in earth ' s surface of deep - action . in nature , it is the consequence resulted by the terranes inserted as strips and blocks , regional transversal structure develope
區(qū)域地球化學(xué)研究表明，包括江達(dá)構(gòu)造帶在內(nèi)的三江構(gòu)造帶北段，區(qū)域地球化學(xué)異常亦表現(xiàn)出北西成帶、北東成條特征，這是深部作用的地表地球化學(xué)響應(yīng)，實(shí)質(zhì)上是地體條塊鑲嵌、區(qū)域橫向構(gòu)造發(fā)育以及與此相關(guān)的殼幔長(zhǎng)期作用的結(jié)果。