1) mafic dikes
基性脉岩
1.
Geochemistry and petrogenesis of the Mesozoic mafic dikes from Shandong Province;
山东中生代基性脉岩的元素地球化学及其成因
2.
The SiO2 content of the mafic dikes from Gan-Hang tectonic belt ranges from 46.
赣杭构造带中西段发育的基性脉岩以辉绿岩为主,SiO2质量分数为46。
2) mafic dike
基性脉岩
1.
Based on the characteristics of REE(rare earth elements) of mafic dikes in western Fujian Province in China,both petrogenetic type and magma evolution mechanism of the rocks were discussed.
利用稀土元素特征对闽西基性脉岩的成岩方式和岩浆演化机制进行探讨。
3) Basic dikes
基性岩脉
1.
Petrochemical characteristics of basic dikes and its geological significance in Taoshan-Zhuguang-Guidong area;
桃山—诸广—贵东地区基性岩脉岩石化学特征及其地质意义
4) mafic dikes
基性岩脉
1.
Geochemistry of the late Mesozoic mafic dikes in western Fujian Province;
闽西晚中生代基性岩脉的地球化学研究
2.
Geological and geochemical characteristics and its significance of mafic dikes from Northwest Jiangxi Province;
赣西北基性岩脉的地质地球化学特征及其意义
3.
The coastal area around Southeastern Fujian is located in the Changle-Nan ao tectonic zone, where mafic dikes (swarms) were developed since late Mesozoic.
闽东南沿海地处长乐-南澳构造带内,发育晚中生代以来的基性岩脉(岩群),其几何形态和产状记录着区域应力场活动。
5) mafic dike
基性岩脉
1.
Mesozoic mafic dikes in Northeast Hunan Province belong to tholeiite series,and part of lamprophyre belongs to alkali basalt series.
湘东北基性岩脉以 K2 O/ Na2 O<1,K2 O+Na2 O在 3。
2.
Mesozoic mafic dikes occurring in Northeast Hunan Province can be divided into two rock types.
湘东北中生代基性岩脉可以分为煌斑岩和辉绿岩两类 ,前者形成于 136 。
6) meso-basic dyke rock
中基性脉岩
1.
For example, magnetic anomalies have been measured on the gold deposits yielded in meso-basic dyke rocks and crash altered volcanic rocks.
许多金矿的赋矿(或伴生)岩石与其周围岩石之间存在着磁性差异,如与中基性脉岩有关的金矿成因模式矿床、破碎蚀变火山岩型金矿等,在其上能观测到磁异常。
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