沉積巖學者 的英文怎麼說
中文拼音 [chénjīyánxuézhě]
沉積巖學者
英文
sedimentationist- 沉 : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
- 積 : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
- 巖 : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
- 學 : Ⅰ動詞1 (學習) study; learn 2 (模仿) imitate; mimic Ⅱ名詞1 (學問) learning; knowledge 2 (學...
- 者 : Ⅰ助詞1 (用在形容詞或動詞後面 或帶有形容詞或動詞的詞組後面 表示有此屬性或做此動作的人或事物) 2 ...
- 沉積 : [地] deposit; sedimentation; deposition; precipitation
- 學者 : scholar; learned man; man of learning
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Perhaps the future role of the sedimentary petrologist will be as an interpreter and an arbiter of cases too complex for the machine to decide unaided.
沉積巖石學家將來的作用也許是作為機械不能獨立解決復雜情況的解釋者和仲裁者。Geophysicists had already cognizance of that the pervasive velocity anisotropy with varying degree in the mantle or the sedimentary rock of upper crust is an important physical property. almost all existed research works fasten on those transversely isotropic media with vertical or horizontal axis of symmetry ( ti ).,
地球物理學者已認識到從地幔到地殼上部的沉積巖存在著不同程度的各向異性,且對具有垂直或水平對稱軸的橫向各向同性介質( ti )有很多的研究。Many studies had attempted to characterize chemical weathering process by focusing on geochemisty of river particulate and sediment. the sediment geochemistry may reflect and compare with the carbonates and silicates weathering degree by introducing the chemical index of alteration ( cia ) and new sediment index of variation ( siv ) and elemental molar abundance ratio of the sediment. the one main objective of this study would provide and compare the relative weathering intensities of silicates and carbonates with the different basins
2沉積物地球化學與化學風化進程和機械剝蝕率化學風化指數與化學風化率屬于表徵化學風化作用意義不同的函數,前者為相對概念反映流域巖石在原巖基礎上己發生淋溶作用的深度,主要受到了氣候因子的深刻影響(中國流域沉積物化學風化指數由北到南呈有規則的遞增序列,氣候因子對風化進程的影響掩蓋了巖性的巨大差異) ,而化學風化率含義是指單位流域面積巖石風化淋溶產生的離子絕對總量。Supervision over china ' s securities market and risk control
中國石油大學沉積巖石學教學及教材建設的奠基者Guided by the basic theory of high - resolution sequence stratigraphy, and based on the core observation, the analysis of chemical composition of rocks, and data of natural potential logging and apparent resistivity logging, authors have set up the high - resolution sequence stratigraphy framework of the ore - hosting yaojia formation, and discussed the relation of the stratigraphic structure of the middle cycle, as well as the paleotopography, the micro - facies to the formation of uranium deposit
在高解析度層序地層學基本理論指導下,筆者通過巖心觀察、巖石化學組分分析、自然電位及視電阻率測井等手段,建立了賦鈾巖系姚家組高解析度層序地層格架,探討了中期旋迴內地層結構、古地形和沉積微相與鈾礦床形成的關系。Based on extensively gathering and sysmatically analyzing much geophysics, sedimentary, structure and petrological materials in research field and taking two field geological explorations from south to north in western odors basin margin, the paper studied large numbers of seismic sections and newly - finished profiles in former seismic blanked area of western margin as well as up - to - date gravity and magmatic fruits, put views on the regional geotectonic background and basin - mountain coupling and made through research on the structure features and attribute together with the result of fission track testing
筆者廣泛收集和系統分析了研究區大量的地球物理、沉積、構造和巖石學等資料,對盆地西緣自南而北進行了兩次野外地質實際調查,在此基礎上,重點研究了大量地震剖面和在西緣地震勘探空白區新完成的地震剖面及新近重磁電研究成果,結合裂變徑跡等測試分析資料,從區域地球動力學背景和盆山耦合的思路入手,對鄂爾多斯盆地西緣的構造特徵及其屬性進行了詳細解剖。Since the long time, different scholars had different viewpoints on stratigraphic succession ^ sedimentary environment and especially chronology evidences of the stratum, that effected infinitely the reconstruction of the tectonic evolutions and paleolithofacies palaeogeography pattern
長期以來,不同學者對該套地層的地層層序、沉積環境、尤其是地層時代歸屬等均存在較大的爭議,給正確恢復該區大地構造演化和巖相古地理格局帶來了極大影響。分享友人