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иxԇ

l(f)r(sh)g:2017-03-17 ݋:

xԇһֱҪLr(sh)gxĿԇ(xing)ĿС@Vôٽиx}soɡ

ԭģ

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, according to 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.

һy~

spatial: a.1.gģ̫յ;2.(߰l(f))g

plume: n.1.2.

xenolith:̔r

percolate:v.1.B͸2.U(ku)ɢ

portions: n.һ

y

1.the best evidence for the layered-mantle thesis is the well-established fact that volcanic rocks found on oceanic islandsislands believed to result from mantle plumes arising from the lower mantleare composed of material fundamentally different from that of the mid-ocean ridge system whose sourcemost geologists contendis the upper mantle.

ڵ᣷֌Փc(din)fõC(j)@һ(g)_J(rn)Œ(sh)ЩuZ——@ЩuZ(j)ԴŒӵρĵ܎r(mantle plume)——ϰl(f)F(xin)Ļɽrʯcвɽϵy(tng)|(zh)ͬ|(zh)(gu)ɵ@һвɽϵy(tng)ij(sh)|(zh)W(xu)Փqϲ

yͣ(f)sZ

ጣǰɲythe evidence is the fact that,yyfact֮ffact ͬλZľˏľмдβZЏľ䣬^yxͬλZľZvolcanic rocksZfound on oceanic islandsǷ~volcanic rocks;islandsһ(g)fislandsͬλZislands believed to result from mantle plumes arising from the lower mantle,ͬλZ(sh)Hһ(g)ָ^ͬλZ^Z(dng)~are composed/of fundamentally different from that of the midocean ridge system, whose source, most geologists contend, is the upper mantle

һЩ~R_²fο@һ(g)t׵layered mantle thesisy⡣x܉xӵĴ˼layered mantle thesisrC(j)fundamentally different from… the upper mantle,@(yng)ԓƜyȻͬόӵt@(g)ՓһfвͬČ

2. some geologistshoweveron the basis of observations concerning mantle xenoliths argue that the mantle is not layeredbut 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 irregularlyaccording to the vagaries of the fluids’ pathways. (4+)

ijЩ|(zh)W(xu)ңԌᣲ̔rw(xenolith)^(j)ָᣲǷ֌е෴ᣵĮ|(zh)Щ“ݳɷ”|(zh)(gu)ɵ@ЩɷڅwǹwĠB(ti)¶ϝB͸U(ku)ɢ@Щ|(zh)ԣҎ(gu)t،ϲᣵijЩԸ׃

yͣ(f)sZ

ጣһ(g)LZhowever, on the basis of observations concerning mantle xenoliths,^ӵҪy߀that(do)eZľľbut Bӵăɂ(g)ӣһm(x)ĩxrich in incompatible elementsfluids;һ(g)ͬλZһ(g)~Y(ji)(gu)incompatible elements߀һ(g)Zǂ(g)~Y(ji)(gu)ӌ^(f)s

½Y(ji)(gu)

Tsµĵһ@һƪǽY(ji)Փ͡_ʼf˵heterogeneous,Ȼָspatial arrangement remains unresolved,Ȼ˃ɷNՓһlayered-mantle thesis,һ(g)irregularly heterogeneous.Ȼքe@ɷNՓM(jn)describe.ָWe believe, perhaps unimaginatively, that this debate can be resolved through further study, and that the underexplored midocean ridge system is the key.

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