实例解析如何攻克GRE阅读中的难词难句

时间:2014-11-15 11:26:45  / 编辑:fairy

  我们在做一篇GRE阅读题的时候,要把握文章重点,通过攻克难词难句高效解题。下面,一诺留学小编就来为大家实例解析,如何攻克GRE阅读中的难词难句,提高阅读能力。

  GRE阅读NO题的NO8-1,我们从“词--句--篇章”来谈谈这篇文章:

  Geologists have long known that the Earth‘s mantle is heterogeneous, but its spatial arrangement remains unresolved—is the mantle essentially layered or irregularly heterogeneous? The best evidence for the layered-mantle thesis is the well-established fact that volcanic rocks found on oceanic islands, islands believed to result from mantle plumes arising from the lower mantle,are composed of material fundamentally different from that of the midocean ridge system, whose source, most geologists contend, is the upper mantle.Some geologists, however, on the basis of observations concerning mantle xenoliths, argue that the mantle is not layered, but that heterogeneity is created by fluids rich in “incompatible elements” (elements tending toward liquid rather than solid state) percolating upward and transforming portions of the upper mantle irregularly, accordingto the vagaries of the fluids’ pathways. We believe, perhaps unimaginatively, that this debate can be resolved through further study, and that the underexplored midocean ridge system is the key.

  一、难词

  spatial: a.1.空间的,太空的;2.存在(或者发生)于宇宙空间的

  plume: n.1.羽状物2.柱,地柱

  xenolith:俘虏岩

  percolate:v.1.渗透2.扩散到,弥漫于

  portions: n.一部分

  二、难句

  1.the best evidence for the layered-mantle thesis is the well-established fact that volcanic rocks found on oceanic islands,islands believed to result from mantle plumes arising from the lower mantle,are composed of material fundamentally different from that of the mid-ocean ridge system, whose source,mostgeologists contend,is the upper mantle.

  对于地幔分层论点来说,最好的证据乃这样一个确认的事实,即在那些海洋岛屿——这些岛屿据信是源于由下层地幔升上来的地幔柱状溶岩流(mantle plume)——上发现的火山岩石,是由与海洋中部山脊系统的物质根本不同的物质构成的,而这一海洋中部山脊系统的成因,大多数地质学家论辩道,为上部地幔。

  以上内容就是实例解析攻克GRE阅读中难词难句的方法,希望考生能熟练掌握。如需了解更多留学考试的相关信息,欢迎拨打一诺留学的免费热线400-003-6508或者010-62680991进行出国留学咨询,或者点击一诺留学官方网站http://www.yinuoedu.net/页面的“在线咨询”与一诺留学专家直接对话。

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