calc-alkaline信息详情
钙碱的
calc───abbr.计算（calculation）
alkaline───adj.碱性的；含碱的
alkaline water───碱性水；碱水
alkaline foods───碱性食品
orifice calc───孔口计算
alkaline battery───[电]碱性电池
cALc uM───钙
calc tufa───石灰华
lifo calc───后进先出计算
Penshan granitic body is a calc-alkaline pluton composed of Muscovite alkali granite, two-mica alkali feldspar granite and biotite adamellite.───彭山岩体是由白云母碱长花岗岩、云母碱长花岗岩和黑云母二长花岗岩组成的钙碱性花岗复式岩体。
The geochemical study shows that the rock is S-type granite, belonging to the calc-alkaline suite.───地球化学特征研究结果表明，嘎若岩体属于钙碱性岩系，为S型花岗岩。
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岩体属富钠的钙碱性系列；
body is a calc-alkaline pluton composed of muscovite alkali granite, two-mica alkali feldspar granite and biotite adamellite.───彭山岩体是由白云母碱长花岗岩、云母碱长花岗岩和黑云母二长花岗岩组成的钙碱性花岗复式岩体。
Qitianling granite is a post - collisional, deep - sourced and hypabyssal, early Yanshanian high - K calc- alkaline granite complex pluton.───骑田岭花岗岩是燕山早期深源浅成的高钾钙碱性复式花岗岩岩体。
Both the Wushi diorite-hornblende gabbros and the surrounding granite-granodiorites belong to high-K calc-alkaline series.───乌石闪长岩角闪辉长岩和周围佛冈黑云母花岗岩、含角闪石花岗闪长岩同属于高钾钙碱性系列岩石。
The Gacun deposit is a typical massive sulfide deposit associated with Late Triassic seafloor calc-alkaline felsic volcanics (VHMS).───呷村矿床是一个与晚三叠世海相钙碱性酸性火山岩系有关的典型块状硫化物（VHMS）矿床。
Geochemistry and petrogenesis of the alkaline and calc-alkaline series Cenozoic volcanic rocks from Huochetou mountain, Tibetan plateau───青藏高原新生代火车头山碱性及钙碱性两套火山岩的地球化学特征及其物源讨论
Genesis of the Xishan high-K calc-alkaline volcanic rocks in South Hunan Province───湘南西山两江口高钾钙碱性火山岩的成因分析
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.