1) bimodal volcanic-intrusive complex rock
双峰式火山-侵入杂岩
2) volcano-intrusive complex
火山岩-侵入杂岩
3) volcanic intrusive complexes
火山-侵入杂岩
4) Volcanic-intrusive complex
火山一侵入杂岩
5) volcanic and intrusive complex rocks
火山侵入杂岩
1.
Based on the studies of the geology,Sm Nd isotopic age and petrology of Gangbian volcanic and intrusive complex rocks from Hengfeng,Jiangxi Province,it is suggested,that the complex rocks were formed at Early Palaeozoic (584±77)Ma ,and belong to calc alkaline series.
通过对赣东北横峰港边火山侵入杂岩的地质学、同位素年代学及岩石学的研究发现，该火山侵入杂岩并非晋宁期岩浆活动的产物，其Ｓｍ－Ｎｄ同位素年龄为（５８４±７７）Ｍａ，归属早古生代。
6) bimodal volcanic rocks
双峰式火山岩
1.
Definition of Neoproterozoic bimodal volcanic rocks in the south of Hangzhou and its tectonic significance;
杭州南部新元古代双峰式火山岩的厘定及其构造意义
2.
The metamorphic rocks consist of three basic-acid volcanic-sedimentary cycles and show the features of bimodal volcanic rocks.
东岩组地层由3个基性、酸性火山喷发 (溢)沉积旋回组成,具有双峰式火山岩特征。
3.
The results showed that the metamorphic volcanic rocks were bimodal volcanic rocks,and its primary rocks were the alkali-basalt and the calc-alkaline rhyolite which both had the similar geochemical characteristics with those of t.
结果表明,矿区变质火山岩为一套以玄武岩为主的双峰式火山岩,其原岩为基性的玄武岩和酸性的流纹岩。
补充资料：3,3'-[氧基双亚甲基]双[3-乙基]氧杂环丁烷
CAS: 18934-00-4
中文名称: 3,3'-[氧基双亚甲基]双[3-乙基]氧杂环丁烷
英文名称: 3,3'-[oxybis(methylene)]bis[3-ethyl-Oxetane
中文名称: 3,3'-[氧基双亚甲基]双[3-乙基]氧杂环丁烷
英文名称: 3,3'-[oxybis(methylene)]bis[3-ethyl-Oxetane
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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