å°åŒ—ç¡¬ç¢Ÿæ•‘æ´ Fundamentals Explained
Consequently, Even though subduction zone rocks can adhere to numerous paths throughout subduction and exhumation, pinpointing the particular route that a specific exhumed subduction zone rock followed is very important for comprehension subduction dynamics.
腦電在。了救資料è¦æƒ³ä¸ä½ 是或,出救經已料資éžé™¤ï¼Œæ©Ÿé–‹çš„次å†è…¦é›»è®“能ä¸ç”Ÿç™¼çš„çœŸä½ è‹¥å€˜ä½†ã€‚è£¡xobpord到放,案檔的è¦é‡æœ€äº›ä¸€å°‡ï¼Œï¿½?è¿°
Data : Web page Pace will be the velocity at which your website responds to instructions input. It is a lot more essential and valuable for your website to have this at a lessen worth. It’s imperative that you work on retaining this speed benefit as reduced as feasible. HTML Details /
+rong �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?鷛
+pian �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?甂
The increasing garnets surrounded these relict minerals as the Click Here garnets grew, plus the relict minerals are preserved as mineralogical evidence of the earlier phase within the metamorphic record on the rock.
+ "u99abu0027u003bu2026ueaf0u0020u0020u0313u0020u3099uff09u208eu2011u2007u2060u000au0020u0020u300bu0bf9",
+cuo �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?é†
+zhi �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?å€ ï¿½?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?瘈
For a few rocks, the only real part of the P-T path recorded inside the mineral assemblage and texture in the rock could be the 'peak' of metamorphism -- the circumstances with the thermal highest (i.e., the utmost temperature as well as force at the maximum temperature). If your rock had a sedimentary or volcanic protolith, you could infer the rock started out on the surface, attained peak disorders at some temperature and depth within the Earth, and returned to your surface area (in which the rock was gathered).
é‡å®¹çš„åŠä¸€æˆè®Šåªéƒ½ç¢Ÿç¡¬ï¿½?G 本原�?了見ä¸å€‹æ•´ä¸‹æ³ç‹€çš„妙其å莫在 槽D的料資多很化å¼æ ¼æœ‰æ²’都弄麼怎明�?é¡Œå•éº¼ä»€äº†å‡ºæ˜¯åº•åˆ°æ¥šæ¸…ä¸æžä¹Ÿæˆ‘尾到
+shi �?�?�?�?什 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?æ€ ï¿½?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?襹
Employing zoning info to reconstruct the Section of the P-T route experienced from the zoned mineral is just not very simple, but a few normal aspects of the relationship of zoning to P-T path may possibly conveniently be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims document growth zoning that represents the modify with the lessen-T circumstances at which the garnet core grew to the upper-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving rising temperature and pressure). Mn is preferentially partitioned into garnet relative to most other common minerals, so Mn is sequestered in early-shaped garnet, depleting the area setting from the expanding garnet in Mn. (b) Minerals that exhibit main factor advancement zoning most likely did not practical experience very high metamorphic temperatures. At superior temperature (> 700 C) and ample period, zoning can be homogenized as intracrystalline diffusion results in being more effective at removing compositional variation.
硬碟 æ ¼å¼åŒ–後�?]想感[]常日[ . 請時�?.æ¯è¨Šï¿½??嗎碟硬化å¼æ ¼è¦åŒ–å¼æ ¼æœªç¢Ÿç¡¬æˆ–åƒæ•¸éŒ¯èª¤ç¾å‡ºæœƒç¢Ÿç¡¬é¡†ä¸€æœ‰ä¸‹åº•ç‚ºï¿½?�?碟硬化å¼æ ¼è‘—急è¦ä¸è«‹æ™‚æ¤.