1) mafic igneous rocks
基性火成岩
1.
Geochemical investigations on late Mesozoic(early Cretaceous)mafic igneous rocks from both areas separated by Tan -Lu Fault show clear geochemical and isotopic zonation.
华北陆块晚中生代(早白垩世)基性火成岩沿着郯庐断裂带存在显著的元素-同位素地球化学分区。
2) intermediate-basic igneous rocks
中基性火成岩
1.
The author believedthat the origin of ilvaite relate to the intermediate-basic igneous rocks and its disintergrate relateto the paticipate in of borium, through the comparison of geological features between theShangqing ilvaite-rich iron deposit,Qinghai,and the Makeng ilvaite-bearing iron deposit, Fu-jian.
通过富含黑柱石的青海省双庆铁矿区与仅含少量黑柱石的福建省马坑铁矿区矿床地质特征的对比,认为矿床中黑柱石的产生与中基性火成岩的参与有关;黑柱石的解体与硼的参与有关。
3) Alkali eruptive rock
碱性火成岩
1.
Nepheiite was generating in Alkali eruptive rock and pegmatite that rich of Na2O and poor of SiO2.
霞石主要生成于富含Na2O而贫SiO2的碱性火成岩及伟晶岩中,晶体呈六方短柱状、厚板状、等粒状集合体或致密块状产出。
5) intermediate igneous rocks
中性火成岩
6) basic volcanic rock
基性火山岩
1.
Geochemistry and tectonic setting of basic volcanic rocks in Ke-Xia region, northwestern Junggar Basin;
准噶尔盆地西北部克-夏基性火山岩地球化学特征及其构造环境
2.
Characteristics and tectonic settings of the Devonian basic volcanic rocks in Mandula, Inner Mongolia;
内蒙古满都拉泥盆纪基性火山岩特征及其形成环境
3.
The geological features,trace elements,REE,sulphur isotope,lead isotope,and mineral inclusions of basic volcanic rock-type copper deposits in eastern Gejiu zone are studied.
通过对个旧东区基性火山岩型铜矿的矿床地质、微量元素、稀土元素、硫同位素、铅同位素及矿物包裹体等的分析表明,区内铜矿床的产出与地层产状一致,其形成与印支期基性火山岩活动可能有着直接的成因关系。
补充资料：连续性与非连续性(见间断性与不间断性)
连续性与非连续性(见间断性与不间断性)
continuity and discontinuity
11an父ux泊g四f“山。麻以角g、.连续性与非连续性(c。nt，n琳t:nuity一)_见间断性与不间断性。and diseo红ti-
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条