1) 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。
2) intermediate igneous rocks
中性火成岩
3) 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。
4) Intermediate-acid igneous rock
中酸性火成岩
1.
There fore, it is very significant to study the evolution and formation of the Tarim Basin- Through systematic investigations of field geology, drilling records, geophysical results and isotope geology, the occurrence of a Permian intermediate-acid igneous rock zone in the northern part of the Tarim Basin has been confirmed.
研究发现塔里木盆地北部发育一条二叠纪中酸性火成岩带，岩性主要有中酸性的安山岩、英安岩、流纹岩、花岗闪长岩、花岗岩、花岗斑岩、凝灰岩等，同位素年代为247。
5) intermediate igneous rocks
中性火成岩<地>
6) intermediate-basic volcanic rock
中基性火山岩
1.
There are not only developed acidic vol- canic rocks but also extensive intermediate-basic volcanic rocks.
徐深气田汪家屯、安达-宋站地区火山岩储层岩性复杂,不仅发育有酸性火山岩,还发育了大面积的中基性火山岩,在对研究区内不同火山岩储层岩性、物性、电性、含气性特征进行系统分析后发现,不同岩性储层"四性"关系特征有很大差异,由于测井响应是岩石成份、孔缝发育程度和流体性质等的综合反映,因此将测井响应与"四性"关系特征相结合,同时应用岩心、测试、录井等资料对研究区内营城组火山岩储层流体性质进行了识别。
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