The Ultimate Guide To 台中硬碟救援

+piao �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?螵

後然 了好修就定不�?式程 復修廠原或階低用再、來回救有果如ataD ~度法沒軌壞

+min �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?錉

+tu �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?嶀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?廜

+chao �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?眧

+heng �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?鑅

+zuo �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?繓

+ "u1781u0b68u0f0cu3010u0085U00011f7au0020u0dd6u200bU000e007au000au2060u2026u002fu2026u24dcu101eu2014u2007u30a5",

+jun �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?袀 �?�?�?菎

For some rocks, the only real Section of the P-T path recorded in the mineral assemblage and texture of your rock could be the 'peak' of metamorphism -- the problems from the thermal maximum (i.e., the most temperature along with the strain at the maximum temperature). Should the rock experienced a sedimentary or volcanic protolith, you'll be able to infer that the rock begun for the surface area, reached peak conditions at some temperature and depth during the Earth, and returned to your surface area Check This Out (exactly where the rock was gathered).

+xuan �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?梋

+hua �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?蘤

+gai �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?峐

+chou �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?簉

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15

Comments on “The Ultimate Guide To 台中硬碟救援”

Leave a Reply

Gravatar