花崗巖狀的 的英文怎麼說
中文拼音 [huāgǎngyánzhuàngde]
花崗巖狀的
英文
eugranitic- 花 : Ⅰ名詞1 (種子植物的有性繁殖器官) flower; blossom; bloom 2 (可供觀賞的植物) flower 3 (形狀像花...
- 崗 : 名詞1. (不高的山) hillock; mound 2. (平面凸起的一長道) ridge; welt; wale3. (崗位;崗哨) post; sentry
- 巖 : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
- 狀 : Ⅰ名詞1 (形狀) form; shape 2 (情況) state; condition; situation; circumstances 3 (陳述事件或...
- 的 : 4次方是 The fourth power of 2 is direction
- 花崗 : granodiorite
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( 4 ) based on the analysis and summary of typical orogenic belt in china, advancing the marker to distinguish the exist of delamination occurred in orogenic belt, especially giving up some new marker such as ring ultrabasic - basic - medium acid rock body, local bimodal continental rifting volcanic activity ; rapakivi granite, etc. ( 5 ) collating the main stages of south part of sanjiang orogenic belts evolution after the close of old nanchangjiang ocean, i
較全面地提出了判別造山帶成熟拆沉作用發生的標志,特別是根據對我國典型造山帶的總結分析,提出了一些新的標志,如環狀超基性一基性一中酸性雜巖體;局部雙峰式大陸裂谷型火山活動;二長花崗巖、堿性花崗巖和奧長環斑花崗巖;地殼局部短暫下沉;等等。This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible
按照不同構造層,研究了各構造層的構造特徵:基底構造層:受早海西期構造作用的影響,與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓構造作用有關,為一構造變形和巖漿侵入活動強烈的古生代褶皺基底。二疊系構造層:受中海西區域性伸展斷陷作用的影響,盆地及其周緣地區發育與伸展構造有關的構造-巖漿組合,如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。All these ductile shear zones are characterized by northward thrusting. the u - pb dating on zircons from the bedded gabbro of the qimanyuter ophiolite melange gives an age of 526 ? 1 ma ( early cambrian )
在其曼于特蛇綠巖的層狀細粒輝長巖中獲得了鋯石u - pb年齡值為526 1ma (早寒武世) ,它被晚奧陶世花崗巖侵入。They are the world s largest globular granite sea stacks
半洋石帆是世界上最大的花崗巖球狀海蝕石柱。Gneissic granite did not experience ultrahigh - pressure metamorphism from bixil
大別山碧溪嶺未經歷超高壓變質的片麻狀花崗巖The steep granite coast is rugged and irregularly stepped, with both up to a metre high vertical faces and narrow shelves often dipping back to retain temporary splash pools. protection of ecological habitats in cape d aguilar marine reserve
該陡斜的花崗石岸崎嶇不平,呈不規則石階狀,有高至1米的垂直面,亦有狹小的巖棚,若海浪涌至,便會形成臨時小水池。The eyes and mouths of hawk - shaped stone are formed by the weathering and eroding of plagioamphibolite or other enclave rocks developing in the adamellite mass while the figure of the hawk is shaped by adamellit mass of taishan group aged 2. 4billion years
24億年左右形成的二長花崗巖中的泰山巖群斜長角閃巖包體,巖石風化剝蝕后形成小孔如老鷹的眼睛和嘴部等,二長花崗巖球狀風化后形成老鷹的外形。The pot shaped peak is formed along the joints and fissures with the weathering and eroding of adamellite formed 2. 4billion years ago
24億年左右形成的古元古代二長花崗巖,沿節理裂隙風化剝蝕后形成的壺狀山峰。In the area without magma mingling or with weak magma mingling, the host rock is dominated by porphyaceous adamellite showing normal granite fabric
無巖漿混合作用或巖漿混合作用較弱區段,寄主巖石以似斑狀二長花崗巖為主,顯示正常的花崗巖結構構造巖漿混合作用強烈區段。Comparing with the granitoid from jiaodong guojialing in mineralogy, the minerals in the granitoid in nimu - qushui granitoid crystallized in the environment of oxidization, the granitoid has a characteristic of rich volatile components and a high content of alkali, the rock - forming minerals and accessory minerals have a characteristic of i - type granite, and the granite shows a characteristic in favor of an and cu ore formation
通過與膠東郭家嶺地區的花崗巖類的礦物學進行對比,可知本區花崗巖類礦物結晶時處于氧化狀態,具有富含揮發分的特徵,堿質含量高,造巖礦物及副礦物表現出型花崗巖特徵,具有殼幔混源物質,表現出有利於金、銅礦形成的花崗巖類的礦物特徵。Wind, water, chemical, and mechanical erosion shaped the granite into their distinctive shapes, revered by aborigines as the eggs of the rainbow serpent
風,水,化學及機械等侵蝕將這些花崗巖塑造成獨一無二的形狀,當地的土著居民將其當作彩虹蛇的卵進行崇拜。The peak looks like profile feature of a buddha quietly lying on the side, which is formed by sphericity and differentiating weathering of adamellite of 2. 4billion years old
24億年左右形成的二長花崗巖組成的山峰,上部巖石發生球狀風化和差異性風化后,遠觀宛如一尊大佛,安靜地側臥。分享友人