The 5-Second Trick For 台中硬碟救援

+zha �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?皻

spiT�?。看玩玩來案檔的要重不個一除刪行自可的試嘗想！單簡此如然居作工檔案救援avuceR ：稱名體�?具工

+jue �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?屩

+ting �?�?�?�?�?�?�?�?�?汀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?榳

+lou �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?謱

- "u2014u0a83ufdfcu003fu00a0u0020u000au2991U0001d179u0020u201dU000125f6u0a67u20a7ufeffu043f",

+hu �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?頀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?焀 �?�?垀 �?�?�?�?�?�?�?�?歑

+kun �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?菎

+lu �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?鏀 �?�?�?�?�?�?�?�?�?�?�?�?鯥

+jian �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?揀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?顅

P-T path form by by itself would not provide a one of a kind interpretation of tectonic procedure or metamorphic driving forces. As an example, clockwise paths can sort in continental collision belts of subduction zones. In the same way, some subduction zone rocks record clockwise paths and a few file counterclockwise paths. Nevertheless, The combination of P-T path features, time/charge data, structural information, and various petrologic data can provide significant information regarding metamorphic and tectonic processes.

+kuang �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?劻

Making use of zoning data to reconstruct the Section of the P-T route experienced by the zoned mineral will not be simple, but a few basic components of the relationship of zoning to P-T path may perhaps effortlessly be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims record progress zoning that signifies the alter through the lower-T situations at which the garnet Main grew to the higher-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving raising temperature and pressure). Mn is preferentially partitioned into garnet relative to most other frequent minerals, so Mn is sequestered in early-shaped garnet, depleting the area surroundings with the escalating garnet in Mn. (b) Minerals that display key factor advancement zoning possibly didn't practical experience very substantial metamorphic temperatures. At high temperature (> seven-hundred C) and sufficient length, zoning may very well be homogenized as intracrystalline diffusion turns into more practical at Clicking Here removing compositional variation.

+tao �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?鞀 �?�?�?�?鋾