近地表巖石 的英文怎麼說
中文拼音 [jìndebiǎoyándàn]
近地表巖石
英文
near-surface rock-
Through the ree charactheristics being studied, it suggests that the xenoliths from hannuoba, ximeng, and puning area have no the trend of lree enrichment, which ratios of lree / hree approximate 1. therefore, it is not different from archean lithospheric mantle
稀土元素地球化學研究表明,漢諾壩、錫盟、普寧等地區包體則無lree富集的趨勢, lree hree接近於1 ,因此它們與太古代巖石圈地幔不同,稀土元素特徵表明它們遭受了強烈虧損。The biosphere, a thin shell that encapsulates the earth, is made up of the atmosphere and lithosphere adjacent to the surface of the earth, together with the hydrosphere
生物圈就像一層包裹著地球的薄的貝殼,它由大氣圈、水圈以及地表附近的巖石圈組成。The karst water moves from south to north. after moving to jinan city, the karst water is blocked by igneous bodies, the karst water passes through fissures and karst and gushes out to the surface as springs
來自南部補給區的巖溶地下水徑流至老城區附近,遇到巖漿巖體阻隔,在地形低洼部位通過淺部石灰巖巖溶裂隙湧出地表,形成濟南諸泉。It was also indicated by the studies on a large number of pb isotope that pb in ores of the deposit chiefly came from volcanic rocks in the strata and later intrusions with derivation of a little pb from the normal deposit stratum
大量pb同位素研究也表明,礦床的礦石鉛源跨越了下地殼、地幔和造山帶演化線,形成混合鉛帶,多集中於地幔和造山帶演化線附近,暗示pb主要來自地層中的火山巖和後期的侵入巖,少量來自正常沉積地層。Submerged rocks are a pinkish-blue hue, while the open water tends to a desaturated blue.
淹沒在水中的巖石呈淺粉紅--藍色調,但地表水接近於不飽和的藍色。Submerged rocks are a pinkish - blue hue, while the open water tends to a desaturated blue
淹沒在水中的巖石呈淺粉紅- -藍色調,但地表水接近於不飽和的藍色。This course covers sediments in the rock cycle, production of sediments at the earth ' s surface, physics and chemistry of sedimentary materials, and scale and geometry of near - surface sedimentary bodies, including aquifers
本課程涉及到巖石循環中的沉積物,在地球表面沉積物的產生,沉積物的物理和化學性質,和近地表沉積體的規模和形狀,包括含水層。Valley and i saw immediately that the magma must have originated in rock once near the earth ' s surface
我們立即了解,該巖漿必定是由近地表的巖石形成。The results show that the weak parts of grottoes often are nearby at the corners of grottoes and that to employ the anchoring steel - bars in the gaps does good to the safety of the whole structure of grottoes
計算結果表明地震作用下薄弱部位多數發生在石窟的角點附近,採用合理的預應力錨索加固技術可以有效提高石窟巖體的抗震安全性。分享友人