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[Issue Essay]

试题详情

题目:

Analytical!

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答案:

提问:

老师您好能否帮我讲解下下面这个文章考试时该如何读,我读完这种文章压根不知道在说什么,只知道在讲ocean basin形成机制的几种理论。No very satisfactory account of the mechanism that caused the formation of the ocean basins has yet been given. The traditional view supposes that the upper mantle of the earth behaves as a liquid when it is subjected to small forces for long periods and that differences in temperature under oceans and continents are sufficient to produce convection in the mantle of the earth with rising convection currents under the mid-ocean ridges and sinking currents under the continents. Theoretically, this convection would carry the continental plates along as though they were on a conveyor belt (conveyor belt: n. 传送带) and would provide the forces needed to produce the split that occurs along the ridge. This view may be correct: it has the advantage that the currents are driven by temperature differences that themselves depend on the position of the continents. Such a back-coupling, in which the position of the moving plate has an impact on the forces that move it, could produce complicated and varying motions. On the other hand, the theory is implausible because convection does not normally occur along lines, and it certainly does not occur along lines broken by frequent offsets (an abrupt bend in an object by which one part is turned aside out of line) or changes in direction, as the ridge is. Also it is difficult to see how the theory applies to the plate between the Mid-Atlantic Ridge and the ridge in the Indian Ocean. This plate is growing on both sides, and since there is no intermediate trench, the two ridges must be moving apart. It would be odd if the rising convection currents kept exact pace with them. An alternative theory is that the sinking part of the plate, which is denser than the hotter surrounding mantle, pulls the rest of the plate after it. Again it is difficult to see how this applies to the ridge in the South Atlantic, where neither the African nor the American plate has a sinking part. Another possibility is that the sinking plate cools the neighboring mantle and produces convection currents that move the plates. This last theory is attractive because it gives some hope of explaining the enclosed seas, such as the Sea of Japan. These seas have a typical oceanic floor, except that the floor is overlaid by several kilometers of sediment. Their floors have probably been sinking for long periods. It seems possible that a sinking current of cooled mantle material on the upper side of the plate might be the cause of such deep basins. The enclosed seas are an important feature of the earth’s surface, and seriously require explanation because, in addition to the enclosed seas that are developing at present behind island arcs, there are a number of older ones of possibly similar origin, such as the Gulf of Mexico, the Black Sea, and perhaps the North Sea.

解答:

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阅读239188
解答: 郭培月

提问:

老师,我今天考试碰到的寂静题,一模一样!然后根本算不出来啊,两个式子结合是30x=5y.不知道寂静答案是怎么算出来x=15 y=90的?

解答:

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阅读240402
解答: ken@boost.org.cn老师

提问:

请May老师解答~ 老师,您回复我的这一题,关于圆心角 和 圆周角,我有几个问题想问: 1. ABC是一个优弧,优弧的圆心角是怎么看的呢?为什么是∠BOC,而不是∠AOC呢? 2. 此图中,(优弧)弧ABC 和 (劣弧) 弧AC是否有同一个圆心角 和 同一个圆周角呢? 如果不是,老师可否分别把此图中 优弧与劣弧的圆心角和圆周角画一下? 2. 优弧ABC所对应的圆周角 是∠E(我用红笔加上去的那一个)吗?

解答:

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阅读240401
解答: 徐小梅老师

提问:

请May老师解答,想问一下鸡精的答案是不是错了?我的解答过程有没有问题?

解答:

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阅读237462
解答: 徐小梅老师

提问:

请May老师解答,这题没有头绪

解答:

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阅读236917
解答: 徐小梅老师

提问:

请May老师解答

解答:

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阅读236509
解答: 徐小梅老师

提问:

请May老师解答

解答:

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阅读235924
解答: 徐小梅老师

提问:

请May老师解答

解答:

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阅读236064
解答: 徐小梅老师

提问:

请May老师解答

解答:

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阅读236476
解答: 徐小梅老师

提问:

请May老师解答

解答:

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阅读236707
解答: 徐小梅老师

提问:

请May老师解答

解答:

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阅读234980
解答: 徐小梅老师

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