例句與造句

1. Classification of tectonic sequence and dynamic evolution of jixi basin , eastern heilongjiang province
   黑龍江東部雞西盆地構(gòu)造層序劃分與盆地動力學(xué)演化
2. Through studying the stratigraphic framework of tectonic sequence , the characteristics of deposits and multi - episode tectonic movements show the eastern qinling and dabie orogenic movement and basin formation processes
   晚白堊世至古近紀(jì)區(qū)域構(gòu)造背景發(fā)生重大變化，構(gòu)造層序記錄了晚燕山期地殼快速均衡隆升，伸展斷陷盆地形成演化過程。
3. Through comparing the tectonic sequences stratum of triassic - paleogene period in the east of hubei , in jingmen - dangyang basin , in zigui basin and in the northeast of sichuan , on the southern margin of the eastern qinling and dabie orogenic belt , three main tectonic sequences are divided
   摘要通過對東秦嶺大別山造山帶南緣鄂東地區(qū)、荊當(dāng)盆地、秭歸盆地和川東北地區(qū)三疊紀(jì)古近紀(jì)的構(gòu)造層序?qū)Ρ妊芯浚瑒澐殖鋈齻€大的構(gòu)造層序，并分析了中上揚子地區(qū)印支期以來沉積盆地性質(zhì)轉(zhuǎn)換和遷移過程與構(gòu)造層序的耦合關(guān)系，揭示了東秦嶺大別造山與成盆作用過程。
4. The investigation in the field was combined with research indoors . by classifying tectonic sequence , confirming corresponding prototype basin , analyzing paleo - tectonic stress fields in different periods , plotting correlative tectonic map based on 297 explore wells , and analyzing the traits of the remaining depressions producing hydrocarbon and their migration rules in the ordovician , the author studied the basement of the basin ; the fault system of the basin ; the tectonic - sedimentary evolution of the basin and its circumference areas ; the prototype basin and corresponding dynamics background ; the paleo - tectonic patte rn and its evolution in the layers of producing gas in different periods of ordovician ; the superposition relationship among the different period basins formed by different stress fields ; the reformation of the basin and the formation , redistribution and final emplacement of the gas pools
   采用野外地質(zhì)調(diào)查與室內(nèi)綜合研究相結(jié)合，通過構(gòu)造層序的劃分及其相應(yīng)盆地原型的確定、不同期次古構(gòu)造應(yīng)力場的分析、以297口探井?dāng)?shù)據(jù)為基礎(chǔ)的相關(guān)構(gòu)造圖件的編制、奧陶系殘余生烴坳陷及其遷移規(guī)律研究等的綜合分析，開展了盆地基底以及盆地斷裂系統(tǒng)、盆地及鄰區(qū)構(gòu)造與沉積演化、盆地原型及其形成的動力學(xué)背景、奧陶系產(chǎn)氣層不同時期的古構(gòu)造格局及其演化、不同期次構(gòu)造應(yīng)力場形成的不同世代盆地之間的疊置關(guān)系以及盆地改造與天然氣藏的形成、重新分配和最終就位諸方面的研究。
5. The basin has three evolutionary stages including intracontinental rift basin in p1 - p2 , down basin in t2 + 3 - k and the strong trust - orogeny process in n - q . according to the unconformity contact relationship and sedimentary components , santanghu basin is divided into four tectonic sequence such as : o - c tectonic sequence of basement , pi - p3 tectonic sequence , t - k tectonic sequence and n - q tectonic sequence
   根據(jù)盆地地層之間的不整合接觸關(guān)系，考慮到各層序沉積物組成與生物組合特征等因素，將三塘湖盆地劃分為： ( o ? c )基底構(gòu)造層序，二疊系( p )構(gòu)造層序，三疊系( t ) ?白堊系( k )構(gòu)造層序和第三系、第四系構(gòu)造層序。
6. It's difficult to find tectonic sequence in a sentence. 用tectonic sequence造句挺難的
7. Some conclusions are listed as follows : the plateform cover cap of ordos basin and its circumference areas can be divided into five tectonic sequences . the tectonic evolution of ordos basin can be classified in six stages : the basement formation phase ( from archeozoic to paleoproterozoic ) ; the aulacogen phase ( from mesoproterozoic to neoproterozoic ) ; the north china continental sea phase ( from sinian to early - paleozoic ) ; the north china intracratonic depression phase ( from late - paleozoic to early mesozoic ) ; large ordos inland basin phase and the formation of independent ordos basin ( mid - late mesozoic ) ; fault basin phase around the ordos basin ( cenozoic )
   通過研究有以下成果及認(rèn)識：鄂爾多斯盆地及其周緣地區(qū)沉積蓋層可劃分為五大構(gòu)造層序，盆地的形成和演化分為六大構(gòu)造階段：太古代至古元古代基底形成階段、中新元古代克拉通內(nèi)裂陷槽或坳拉槽演化階段、震旦紀(jì)?早古生代華北陸表海盆演化階段、晚古生代?早中生代華北克拉通坳陷演化階段、中生代中晚期大鄂爾多斯內(nèi)陸盆地演化階段及獨立鄂爾多斯盆地的形成、新生代周緣斷陷盆地演化階段。