Hirano Naoto, Takahashi Eiichi, Yamamoto Junji, Abe Natsue, Ingle Stephanie P, Kaneoka Ichiro, Hirata Takafumi, Kimura Jun-Ichi, Ishii Teruaki, Ogawa Yujiro, Machida Shiki, Suyehiro Kiyoshi
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro, Tokyo 152-8551, Japan.
Science. 2006 Sep 8;313(5792):1426-8. doi: 10.1126/science.1128235. Epub 2006 Jul 27.
Volcanism on Earth is known to occur in three tectonic settings: divergent plate boundaries (such as mid-ocean ridges), convergent plate boundaries (such as island arcs), and hot spots. We report volcanism on the 135 million-year-old Pacific Plate not belonging to any of these categories. Small alkalic volcanoes form from small percent melts and originate in the asthenosphere, as implied by their trace element geochemistry and noble gas isotopic compositions. We propose that these small volcanoes erupt along lithospheric fractures in response to plate flexure during subduction. Minor extents of asthenospheric melting and the volcanoes' tectonic alignment and age progression in the direction opposite to that of plate motion provide evidence for the presence of a small percent melt in the asthenosphere.
离散板块边界(如大洋中脊)、汇聚板块边界(如岛弧)和热点。我们报告了1.35亿年前太平洋板块上不属于上述任何一类的火山活动。小型碱性火山由少量熔体形成,起源于软流圈,这从它们的微量元素地球化学和惰性气体同位素组成可以推断出来。我们认为,这些小火山是在俯冲过程中因板块弯曲而沿着岩石圈断裂喷发的。软流圈少量熔融的程度较低,以及火山的构造排列和年龄在与板块运动方向相反的方向上的递进,为软流圈中存在少量熔体提供了证据。