有人有興趣一起組網路讀書會嗎？

[macaca]

各位IBT戰友們:

想要組個網路讀書會 來分攤消化新橘寶書中的內容。
橘寶書的內容很多 但是多半是中文的 不是很能心安
所以之前我的方法都是去WIKIPEDIA或是GOOGLE找相關的英文知識來消化

可是ㄧ個人進展有點慢
所以想找有興趣的朋友一起來幫忙
尤其是如果大家找自己熟悉的領域 就可以更有效率
(因為更容易準確的用關鍵字搜尋)
如果你也願意 就請把你找到的相關知識放在檔案庫中，順便可以分享給其他的戰友們~

在下預計十二月初要考(報名了兩次)，所以陸續會先把目前找好的相關資料放上來 讓大家參考，也歡迎朋友們一起加入分攤的工作，為了避免重複，我們可以先把自己預計要做的頁數或是主題PO在板上。另外，為了尊重橘寶書的作者著作權，我們僅將自己找到的網路相關知識PO出來就好，不將橘寶書的內容PO出(我想相關的JJ 應該很多網路上都找的到 :P)

若有興趣的戰友 就麻煩在樓下出個聲 感激感激~
因為我是唸生物的，所以想在11/6前整理完70-86頁閱讀生物學的部分。
大家ㄧ起來打倒萬惡ETS的關卡。

以下是個人的整理方式 歡迎大家參考使用 !
主題: 板塊構造學說
新橘寶書頁數: 49 類型: 閱讀 分類: 自然科學:GEOLOGY

英文:
Plate tectonics (from Greek τέκτων, tektōn "builder" or "mason") is a theory of geology that has been developed to explain the observed evidence for large scale motions of the Earth's lithosphere. The theory encompassed and superseded the older theory of continental drift from the first half of the 20th century and the concept of seafloor spreading developed during the 1960s.
The outermost part of the Earth's interior is made up of two layers: above is the lithosphere, comprising the crust and the rigid uppermost part of the mantle. Below the lithosphere lies the asthenosphere. Although solid, the asthenosphere has relatively low viscosity and shear strength and can flow like a liquid on geological time scales. The deeper mantle below the asthenosphere is more rigid again. This is, however, not due to cooler temperatures but due to high pressure.
The lithosphere is broken up into what are called tectonic plates—in the case of Earth, there are seven major and many minor plates (see list below). The lithospheric plates ride on the asthenosphere. These plates move in relation to one another at one of three types of plate boundaries: convergent or collision boundaries, divergent or spreading boundaries, and transform boundaries. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along plate boundaries. The lateral movement of the plates is typically at speeds of 0.65 to 8.50 centimeters per year.
出處: http://en.wikipedia.org/wiki/Plate_tectonics

中文:
板塊構造論，或稱「板塊構造假說」、「板塊構造說學」或「板塊構造學」，是為了解釋大陸漂移現象而發展出的一種地質學理論。該理論認為，地球的岩石圈是由板塊拼合而成；全球分為六大板塊（1968年法國勒皮順劃分），海洋和陸地的位置是不斷變化的。根據這種理論，地球內部構造的最外層分為兩部分：外層的岩石圈和內層的軟流圈。這種理論基於兩種獨立的地質觀測結果：海底擴張和大陸漂移。
出處: http://zh.wikipedia.org/w/index.php?tit ... iant=zh-tw