岩浆与伟晶在地球化学上都近似洋岛玄武岩(Oceanic Island Basalt)，但从 地质证据上来看，澎湖及台湾西部早在渐新世开始张裂，火成活动呈线性分部以 及后来受到板块挤压而结束于晚中新世，这些地...
基于14个网页-相关网页
... oceanic heat flow ==> 海洋热流 oceanic island basalt ==> 海岛玄武岩 oceanic layer ==> 大洋层 ...
基于1个网页-相关网页
oceanic-island basalt 洋岛型玄武岩
oceanic island basalt detail 海岛玄武岩
oceanic island alkali basalt 洋岛型碱性玄武岩
The Early Jurassic alkali basalts from the Riajunlama region probably represent the oceanic island basalt within the plate of the Bangong-Nujiang ocean.
早侏罗世碱性玄武岩代表了班公湖-怒江洋内的板内洋岛玄武岩。
参考来源 - 羌塘地体中生代构造演化：来自火山岩年代学、地球化学及同位素的证据·2,447,543篇论文数据，部分数据来源于NoteExpress
Association of continental alkaline basalt with oceanic tholeiite and oceanic island basalt in the junction is reasonably interpreted.
较合理地解释了结合带内，大洋拉斑玄武岩、洋岛玄武岩、大陆碱性玄武岩共存的地质特征。
The oceanic island basalt is represented by the Nonghuai pillow lava, which is, originally Hawaii type one in the Paleotethyan ocean, an allochthon in the Indosinian foreland fold and thrust belt.
洋岛玄武岩以弄槐枕状熔岩为代表性火山岩，原为古特提斯洋盆中的夏威夷型洋岛，现保存在印支期前陆褶皱冲断带的一个外来岩席中。
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