1) carbonatite-alkalic complex
碳酸岩-碱性杂岩
1.
Mianning-Dechang Himalayan REE belt associated with carbonatite-alkalic complex in eastern Indo-Asian collision zone,southwest China:Geological characteristics of REE deposits and a possible metallogenic model;
REE成矿作用与喜马拉雅期碳酸岩-碱性杂岩体有关,受印度-亚洲大陆碰撞带东部一系列新生代走滑断裂系统控制。
2) alkaline rock-carbonatite complex
碱性-碳酸岩杂岩
3) alkalic carbonatite
碱性碳酸岩
4) ultrabasic complex
超基性岩-碳酸岩杂岩体
1.
A super-large vermiculite-apatite deposit originated from the Qieganbulak ultrabasic complex and located at Southern Kuluketage fault block,northeastern margin of Tarim.
产有超大型蛭石-磷灰石矿床的且干布拉克超基性岩-碳酸岩杂岩体位于塔里木板块东北缘库鲁克塔格断隆南侧。
5) alkaline complex
碱性杂岩
1.
Mineralogy of Taxkorgan Cenozoic alkaline complex in Xinjiang and its implication to pluton genesis;
塔什库尔干新生代碱性杂岩造岩矿物化学成分及成因意义
2.
Through an integrated study of K-Ar chronology, petrology, trace element and, rare earth element geochemistry as well as Sr-Nd-Pb isotope geochemistry on the complex of Yao′an in Yunnan province, the results indicate that: 1) the alkaline complex includes ultrabasic, basic, intermediate and acid rocks; 2) their petrochemistry is characterized by high alkali (Na2O+K2O=6.
对云南省姚安碱性杂岩体的K-Ar年代学、岩石学、岩石化学、微量元素、稀土元素和Sr、Nd、Pb同位素组成等进行了综合研究表明(1)该碱性杂岩体的岩性从超基性、基性、中性到酸性;(2)各类型岩石化学成分均富碱(Na2O+K2O=6。
3.
And many diamond deposits, which are of economic value, have been discovered in the alkaline complex regions.
迄今为止,对金刚石矿床的研究已取得了新的进展,国内外学音认为:“金伯利岩不是金刚石矿床的唯一母岩”,并且在碱性杂岩体中发现了许多具有工业价值的金刚石矿床。
6) alkaline complex
碱性杂岩体
1.
Gold mineralization of these two deposits occurs within the Archean metamophic rocks of Sanggan Group and Hercynian alkaline complex , respectively.
小营盘金矿产于太古宇桑干群变质岩中,东坪金矿产于海西期碱性杂岩体中。
补充资料:碱性岩
碱性岩 alkalic rock 火成岩的一种 。二氧化硅含量较低 ,碱质含量较高(Na2O+K2O> Al2O3 ) 。一般呈浅灰 、浅绿或浅红色。主要浅色矿物为碱性长石(微斜长石、正长石、钠长石),暗色矿物为霓石、霓辉石、钠铁闪石、钠闪石等,副矿物有方钠石、锐钛矿和磷灰石等。可分为深成碱性岩,如霞石正长岩;浅成碱性岩,如霞石正长斑岩;喷出碱性岩,如响岩等。一般产在地壳构造运动较弱的稳定地区,很少形成独立岩体,多与基性岩、超基性岩、碱性正长岩、碳酸岩一起形成杂岩体。与之有关的矿产有铌、锆、稀土、铁、钛、磷等。可利用其钾含量高、二氧化硅含量低的特点,制作化肥和陶瓷原料。 |
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