mesoproterozoic 中文意思是什麼

mesoproterozoic 解釋
中元古代
  1. The grenville - aged orogen is a tie to link most of the continental blocks in rodinia, which existed during the period from late mesoproterozoic through early neoproterozoic

    Grenville期造山帶存在於中晚元古代,是連接rodinia各陸塊的紐帶。
  2. The simulation of mesoproterozoic tectonic stress field forming mafic dyke swarms in the central north china craton

    華北克拉通中元古代巖墻群形成的構造應力場數值模擬
  3. The round columnar joints show that the dyke swarms are in upper crust brittle tectonic setting, and the western shandong block is brittle extensional in the mesoproterozoic time

    巖墻發育圓柱狀節理表明巖墻侵位時地塊已經處于上地殼脆性構造環境,中元古代魯西地區是一個脆性伸展的大地構造環境。
  4. 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識:鄂爾多斯盆地及其周緣地區沉積蓋層可劃分為五大構造層序,盆地的形成和演化分為六大構造階段:太古代至古元古代基底形成階段、中新元古代克拉通內裂陷槽或坳拉槽演化階段、震旦紀?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。
  5. Stratum composition in xiaoqinling represents early precambrian crystal basement and mesoproterozoic era cover rocks of the typical north china craton

    小秦嶺區內地層具有典型華北型早前寒武結晶基底和中元古代以來的蓋層結構,不發育晚古生代、中生代構造層。
  6. The mesoproterozoic wumishan formation in jixian, tianjin represents a succession of 300 - m thick carbonate strata, in which stromatolite biostromes and clotted bioherms are best developed

    天津薊縣中元古界霧迷山組為一套厚3000餘米的碳酸鹽巖地層,疊層石生物層和凝塊石生物丘特別發育。
  7. The minerogenetic epoch lasted from paleoarchean to sinian, with neoarchean, paleoproterozoic and mesoproterozoic - qingbaikouan being the culmination periods

    成礦時代從古太古代到震旦紀,但以新太古代、古元古代、中元古代青白口紀3個地質時期為成礦高峰期。
  8. The mesoproterozoic mafic dyke swarms are extensively distributed in the central north china craton, which are not deformed and metamorphic, emplacing the pre - existed fractures, so the dyke swarms become the conspicuous marks to reconstruct the mesoproterozoic tectonic stress field of the central ncc. the mafic dykes in the northern block are transtensional while the dykes in the central and southern blocks are extensional. the mesoproterozoic tectonic stress field could be simulated on the analysis of the distribution and mechanical origin of the mesoproterozoic mafic dyke swarms in the central ncc. the simulation result shows that the mafic dyke swarms were formed in the extensional tectonic setting in the ncc in the mesoproterozoic time, which are related to the extension of the mesoproterozoic yanliao - zhongtiao aulacogens cross the central ncc

    克拉通北部地塊的鎂鐵質巖墻群為張剪性,而中部和南部地塊為張性。根據華北克拉通中部中元古代鎂鐵質巖墻群的分佈和成因機制分析,來恢復模擬中元古代的構造應力場。數值模擬結果表明鎂鐵質巖墻群在中元古代形成於伸展的大地構造背景,與橫穿華北克拉通中部的燕遼-中條拗拉槽系的伸展作用有一定的聯系。
  9. The geochemical characters of the gaoyuzhuang and yangzhuang formations of mesoproterozoic in pingquan county, hebei province

    河北平泉中元古代高於莊組和楊莊組地球化學特徵
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