ChaseDream
搜索
返回列表 发新帖
楼主: XYXB
打印 上一主题 下一主题

2009年10-11月阅读寂静整理(截至11/18 01:00-The end-Thanks all)

[精华] [复制链接]
31#
发表于 2009-10-22 02:12:00 | 只看该作者
太感谢LZ了!!!
32#
发表于 2009-10-22 02:33:00 | 只看该作者

XYXB,真得很谢谢你,从上个月看你整理到现在,跟噩梦一样,无论如何我明天还是会去的。

就不reschedule了,希望能借点你的好RP,哈哈

33#
发表于 2009-10-22 03:58:00 | 只看该作者

打开是空的

为啥打开是空的呀?可以麻烦发到我的邮箱吗?cindypalau[在] yahoo.com 谢谢了。
34#
发表于 2009-10-22 07:09:00 | 只看该作者
饮水思源。楼主及CD的哥哥姐姐们,你们辛苦了。
35#
发表于 2009-10-22 08:20:00 | 只看该作者
18题背景:
http://www.jcckc.net/geog/AL/Plate/volcano.htm

Vulcanicity and Plate Movement火山作用與板塊移動

The term ‘volcanology’ covers all the processes that molten rock material or magma rises into the crust, or is poured out on its surface, there to solidify as a crystalline or a semi- crystalline rock. And extrusive can be know as volcanic, that the volcanic vlucanicity, when associating with plate movement with reference to destructive plate margins, that the convergent plate margins.
火山作用是熔岩從上地幔流出地面。在地面冷卻形成不同的地形,如火山等。
Actually, most of the earth’s active and dormant volcanoes are associated with constructive, destructive, and some are related to transform plate margins. Although material in the mantle has a high temperature, it is kept in a semi-solid state because of the great pressure exerted upon it. However, if this pressure is released locally by folding, faulting or other movements at plate margins. Some of the semi-solid material becomes molten and rises, forcing its way into weaknesses in the crust, or onto the surface, where it cools, crystallizes and solidifies.
火山帶主要分佈在擴張性、擠壓性及穩定性板塊邊界。因為熔岩受壓,從地殼的裂縫向地面流出。 
1.    At destructive plate margin, the plates converge. Volcanoes, offshore volcanic island arcs are found, e.g. along Circum-Pacific Ring of Fire.
在環太平洋帶上,兩板塊碰撞。火山、離岸火山島孤在板塊邊界上形成。
Circum-Pacific is the ring around the Pacific Ocean basin. In South America, it includes Mountain Andes. In the Western Part of Pacific Ocean, the volcanic islands lie well offshore the North of Pacific Ocean to the Equator and form a chain of island called island arc. The islands include Alentians, Kurils, Japan, the Philippines, and other smaller islands. This island arc is the result of active volcanic activity. It is also called the ‘Ring of Fire’.
The mountain chain is formed at the Eurasian-Indonesian belt, it starts from the west of Alps and is across the Southern part of Europe and extends to the Himalayas. It is the inactive volcanic belt.
The crust is destroyed and mountain is built by the tectonic activities. The tectonic activities are active at the convergent zones that are produced by the compressing force. The radioactive energy is released in the earth’s core. The hot magma rises from the core to the upper mantle. The plates are pushed towards. The denser and thinner oceanic crust is drawn beneath under the continental crust. The edge of the oceanic crust is melted and the pressures increase. The magma flows out along the cracks while the plates collide. The volcanic island is formed along the divergent plate margins. At this subduction zone, the crust is destroyed and the volcanoes are formed. It implies that the plates are unstable.
因為地殼碰撞,大洋板塊向地幔俯衝,形成俯衝帶。因為岩漿受壓沿地殼的裂縫噴出,形成火山或火山島。
2.    At constructive plate margins, the plates diverge. Submarine volcanoes, lava flows, volcanic islands are found, e.g. along Mid-Atlantic Ridge.
在建設性板塊邊界上,兩板塊分離移動。在大西洋中脊上,海底火山、火山島及熔岩流形成。
Due to the tension force, the plates become unstable. The eruption of volcanoes is the major processes and geologic phenomena that are found at the divergent plate margins. When the plates move apart. It is because the heat is released from the earth’s core. While the crust is cracked, the magma flows out from the fissure on the earth’ surface as lava. When the lava is cooled and solidified. After the several eruptions, the volcanoes are formed. At the Mid-Atlantic Ridge, the plates move apart. The magma rises from the mantle and flows out to the ocean floor. The chain of volcanic islands are found along the plate margins. As the plates move, the crust is fracturing. The transform faults are also found.
地殼受張力作用下,兩板塊分離移動。因為岩裝受壓,沿地殼的裂縫流出。因為熔岩受冷及凝固,形成火山島。在大西洋中脊上,地殼受壓破裂,有斷層出現。
Conclusion
Therefore, volcanoes are formed because the plates move apart or towards. It implies that the plates are not stable. The lands are destroyed or the new crusts are formed. The fracturing and folding are actively occurred.
火山及火山島在擴張性、擠壓性等板塊邊界上形成。這些板塊構造地形顯示出板塊在不穩定的情況下,板塊出現了移動,各種地形形成。

By Amethyst Cheung

[此贴子已经被作者于2009/10/22 8:22:18编辑过]
36#
发表于 2009-10-22 08:37:00 | 只看该作者

看到LZMM这个月还总结阅读,好开心~~

37#
发表于 2009-10-22 09:01:00 | 只看该作者
老大效率真高,不过要早睡哦
38#
发表于 2009-10-22 09:11:00 | 只看该作者
为所有奋斗在GMAT一线的童鞋们和所有无私奉献的JJ整理者们致以最崇高的敬意    偶29号一战 顺便为自己祈福 
39#
发表于 2009-10-22 09:12:00 | 只看该作者

拜谢楼主!

40#
发表于 2009-10-22 09:51:00 | 只看该作者

猛然发现昨天换了题库@.@  今天考试呢

您需要登录后才可以回帖 登录 | 立即注册

Mark一下! 看一下! 顶楼主! 感谢分享! 快速回复:

手机版|ChaseDream|GMT+8, 2024-10-1 02:14
京公网安备11010202008513号 京ICP证101109号 京ICP备12012021号

ChaseDream 论坛

© 2003-2023 ChaseDream.com. All Rights Reserved.

返回顶部