青年中文calc-alkaline的意思
calc-alkaline中文翻譯：
鈣堿的
calc───abbr.計算（calculation）
alkaline───adj.堿性的；含堿的
alkaline water───堿性水；堿水
alkaline foods───堿性食品
orifice calc───孔口計算
alkaline battery───[電]堿性電池
cALc uM───鈣
calc tufa───石灰華
lifo calc───后進先出計算
Penshan granitic body is a calc-alkaline pluton composed of Muscovite alkali granite, two-mica alkali feldspar granite and biotite adamellite.───彭山巖體是由白云母堿長花崗巖、云母堿長花崗巖和黑云母二長花崗巖組成的鈣堿性花崗復式巖體。
The geochemical study shows that the rock is S-type granite, belonging to the calc-alkaline suite.───地球化學特征研究結果表明，嘎若巖體屬于鈣堿性巖系，為S型花崗巖。
The major element characteristics show that the intrusion belongs to the sodian calc-alkaline series.───主量元素特征表明卡拉塔格巖體屬富鈉的鈣堿性系列；
body is a calc-alkaline pluton composed of muscovite alkali granite, two-mica alkali feldspar granite and biotite adamellite.───彭山巖體是由白云母堿長花崗巖、云母堿長花崗巖和黑云母二長花崗巖組成的鈣堿性花崗復式巖體。
Qitianling granite is a post - collisional, deep - sourced and hypabyssal, early Yanshanian high - K calc- alkaline granite complex pluton.───騎田嶺花崗巖是燕山早期深源淺成的高鉀鈣堿性復式花崗巖巖體。
Both the Wushi diorite-hornblende gabbros and the surrounding granite-granodiorites belong to high-K calc-alkaline series.───烏石閃長巖角閃輝長巖和周圍佛岡黑云母花崗巖、含角閃石花崗閃長巖同屬于高鉀鈣堿性系列巖石。
The Gacun deposit is a typical massive sulfide deposit associated with Late Triassic seafloor calc-alkaline felsic volcanics (VHMS).───呷村礦床是一個與晚三疊世海相鈣堿性酸性火山巖系有關的典型塊狀硫化物（VHMS）礦床。
Geochemistry and petrogenesis of the alkaline and calc-alkaline series Cenozoic volcanic rocks from Huochetou mountain, Tibetan plateau───青藏高原新生代火車頭山堿性及鈣堿性兩套火山巖的地球化學特征及其物源討論
Genesis of the Xishan high-K calc-alkaline volcanic rocks in South Hunan Province───湘南西山兩江口高鉀鈣堿性火山巖的成因分析
The Penshan granitic body is a calc-alkaline pluton composed of muscovite alkali granite, two-mica alkali feldspar granite and biotite adamellite.
The (examination) of the petrography shows that the volcanic terrains in Tengchong are typical of the basalt-(andesite)-(dacite) arc volcanic rock associations of the calc-alkaline series.
Major elements show that lamprophyres in the orefield are alkalic series and potassic calc-alkaline lamprophyres.
The Fogang granitoid complex is the largest Late Mesozoic batholith in Nanling region, and the Wushi diorite-hornblende gabbros are the most basic end-member of Fogang calc-alkaline series rocks.
Major and trace elements show that the pluton has transition features from high-K calc-alkaline or high- fractionated I-type granites to A-type granites.
The results show that the Triassic SPIRs in the area studied belong to high potassic calc-alkaline series, which were formed in the post-collision setting during Indosinian orogeny.