faulted basin造句
例句與造句
- The chezhen depression as a fault basin is located in the northeastern part of the bohaiwan basin in shandong
摘要車(chē)鎮(zhèn)凹陷古近系沙河街組三段上亞段二段下亞段是較為典型的深斷陷型三級(jí)層序。 - Santanghu basin is a congruent & reconstruct innertief , which developed on the basis of rift - fault basin of permian
三塘湖盆地是一個(gè)在二疊紀(jì)裂谷-斷陷盆地基礎(chǔ)上發(fā)展起來(lái)的疊合、改造型山間盆地。 - Hegang coal field , of the type of a ( inland ) faulted basin far from the sea , was formed in the early neo - jurassic age about 140 million years ago
鶴崗煤田約形成于一億四千多萬(wàn)年前的晚侏羅世初期，是遠(yuǎn)海內(nèi)陸斷陷盆地型煤田。 - Lying in the east of heilongjiang province , yishu graben is a cenozoic fault basin comprising two large second - class structural units , i . e . , tangyuan and fangzheng fault basins
摘要依舒地塹位于黑龍江省東部，為新生代斷陷盆地，湯原斷陷和方正斷陷為其兩個(gè)面積較大的二級(jí)構(gòu)造單元。 - The sedimentary geochemistry analysis indicates that the middle and lower yangtze basin is the craton basin , and shangrao and mingxi basins are the continental margin fault basins in the early triassic
早三疊世的中下?lián)P子混積盆地屬克拉通邊緣盆地，而上饒和明溪碎屑巖盆地則為大陸邊緣斷陷盆地。 - It's difficult to find faulted basin in a sentence. 用faulted basin造句挺難的
- Niuxintuo area in liaohe depression is a fault basin , tectonic movement is complex and fault is developed at the basement and at the late stage , where the conditions for creating various hydrocarbon reservoirs are provided
摘要遼河坳陷牛心坨地區(qū)為斷陷湖盆，基底及后期的構(gòu)造活動(dòng)復(fù)雜，斷層發(fā)育，具有形成各類(lèi)隱蔽油氣藏的地質(zhì)條件。 - In the present survey and valuation the area is divided into three parts : exposed karst region in upwarped distric , karst region controlled by folded structures near depressed belts and blinded karst region in fault basins
目前開(kāi)展的可有效利用的地下水資源調(diào)查評(píng)價(jià)將該區(qū)劃分為隆起帶裸露巖溶分布區(qū)、沉降帶邊緣褶皺構(gòu)造控制巖溶分布區(qū)和斷陷盆地隱伏巖溶分布區(qū)。 - The fault at the east boundary of tangyuan fault basin is a basin - controlling fault , and the faults at both the east and the west boundaries of fangzheng fault basin are also a basin - controlling fault , with the west boundary fault at fangzheng being the major one
斷層的生長(zhǎng)指數(shù)分析表明，依舒地塹內(nèi)部的北西向斷裂與邊界斷裂的活動(dòng)具有一致的規(guī)律性，都起到協(xié)調(diào)邊界斷裂演化發(fā)展的作用。 - According to granite ages cutting ruptures , mineralized quartz veins ages corresponding to fold deformation and formation ages of bilateral faulted basin , deformation age are limited , that are 100 ~ 65ma for one and form 65ma to the present for two and three
根據(jù)斷裂截切的花崗巖體年齡、同期褶皺變形的含礦石英脈年齡以及斷裂兩側(cè)斷陷盆地的形成時(shí)代，大致限定第1期變形時(shí)代為100 65ma ，第2 、 3期變形時(shí)代為65ma現(xiàn)今。 - Compared with lehua manganese deposit in pingxiang - leping faulted basin , which is a sedimentary hydrothermal superimposed type , both orebodies are different obviously in orebody scale , ore type and tenor of manganese etc . , it should be a deposit with different genetic type
并與萍一樂(lè)斷陷盆地內(nèi)的沉積加熱液疊改型樂(lè)華錳礦床進(jìn)行了對(duì)比分析，二者在礦體規(guī)模、礦石類(lèi)型、錳品位等方面存在顯著差別，應(yīng)屬不同成因類(lèi)型的礦床。 - The environment is favorable for the formation oil and gas ; ( 4 ) although the sedimentary environment in the two basins is cardinally identical , the evolution and difference in climate and sedimentary environemt decided the divergence of biotic characters in the two fault basins , and then the biota controlled the type and quality of fossil fuel
盡管兩大盆地在沉積環(huán)境的演化上大體一致，但氣候和沉積環(huán)境的演變和差異決定了兩大斷陷盆地生物面貌上的差異，從而直接控制了化石燃料形成的類(lèi)型和質(zhì)量。 - 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(guò)研究有以下成果及認(rèn)識(shí)：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(dú)立鄂爾多斯盆地的形成、新生代周緣斷陷盆地演化階段。