美国研究生入学考试难句解读-1
时间：2019-02-06 作者：英语课 分类：英文语法词汇
英语课
Most striking among the many asymmetries evident in an adult flatfish is eye placement: before
maturity one eye migrates, so that in (10) an adult flatfish both eyes are on the same side of the head.
在一条成年比目鱼身上显著存在的诸多不对称（asymmetry）特征中，最为吸人注目的是眼睛的摆位：在成年之前，一只眼睛发生移动，因此在成年比目鱼身上，两只眼睛均位于头部的同一侧面。
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
(10) 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.
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。 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
(20) elements" (elements tending toward
liquid rather than solid state)
percolating upward and transforming
portions of the upper mantle
irregularly, according to the vagaries
(25) of the fluids’ pathways.
但是，某些地质学家，以对地幔捕虏岩体（xenolith）所作的观察为依据，指出地幔并非是分层排列的，相反，地幔的异质性是由那些富含“不相容成分”的流质构成的，这些成分趋向于流体而非固体的状态，自下而上渗透扩散，并依照这些流质流向的任意性，不规则地将上部地幔的某些部分予以改变。
maturity one eye migrates, so that in (10) an adult flatfish both eyes are on the same side of the head.
在一条成年比目鱼身上显著存在的诸多不对称（asymmetry）特征中，最为吸人注目的是眼睛的摆位：在成年之前，一只眼睛发生移动，因此在成年比目鱼身上，两只眼睛均位于头部的同一侧面。
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
(10) 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.
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。 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
(20) elements" (elements tending toward
liquid rather than solid state)
percolating upward and transforming
portions of the upper mantle
irregularly, according to the vagaries
(25) of the fluids’ pathways.
但是，某些地质学家，以对地幔捕虏岩体（xenolith）所作的观察为依据，指出地幔并非是分层排列的，相反，地幔的异质性是由那些富含“不相容成分”的流质构成的，这些成分趋向于流体而非固体的状态，自下而上渗透扩散，并依照这些流质流向的任意性，不规则地将上部地幔的某些部分予以改变。