硬碟 程å¼ä¿®å¾© scitsongaiD nretseW:】稱å案檔�?psbn& ;psbn&;psbn&;psbn&;psbn&;psbn&;psbn&.v å¼ç¨‹å¾©ä¿®è»Œå£žç¢Ÿç¡¬DW ;psbn&;psbn&;psbn&;psbn&;psbn&;psbn&;psbn&;psbn&;psbn&;psbn&;psbn&;psbn&;psb
+ren �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?鵀 �?�?�?�?�?�?�?�?牣
+die �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?蹀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?跮
+ "u1806u060du30f5u00b4u17e9u2544u2028u2024u2011u20a3u002du09ccu1782u000duff6fu0025",
+dong �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?è€ ï¿½?�?�?�?�?�?�?�?�?�?駧
+liang �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?倞
+jia �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?鉀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?貑
+ "u1781u0b68u0f0cu3010u0085U00011f7au0020u0dd6u200bU000e007au000au2060u2026u002fu2026u24dcu101eu2014u2007u30a5",
+gan �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?涻
Some inclusions Do not contain lots of information about P-T problems since the minerals are steady over these types of a variety of circumstances (for instance: quartz). Other mineral inclusions are really handy for inferring P-T circumstances and route segments, especially if these minerals no more exist from the matrix with the rock (which is, outdoors the garnet).
您說的情æ³ï¼Œè³‡æ–™å¯ä»¥å›žå¾©ã€‚æˆ‘å€‘çš„æ”¶è²»åƒ¹æ ¼åœ¨æˆ‘å€‘ç¶²ç«™æœ‰æ˜Žç¢ºå ±åƒ¹ï¼Œå¯ä»¥é–‹ç™¼ç¥¨ï¼Œæ²’有å•é¡Œï¿½?資料救æ´ä¸å¿ƒ
+ping �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?鵧
paths The idealized check out of P-T paths is always that mineral assemblages equilibrate at each and every stage of the path within the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This perspective ignores kinetic things related to the energetics of nucleation and advancement of minerals, While these aspects could possibly be significant for a few metamorphic phases and reactions. For instance, the presence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T problems equivalent to The steadiness industry of sillimanite illustrates which the sluggish kinetics of the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outdoors its balance area. It is important to acknowledge the affect of deformation on metamorphic reactions, and the extent to å°ä¸ç¡¬ç¢Ÿæ•‘æ´ which deformation (pressure Vitality) may aid reactions.
- "u002fu2563u202fu0085u17d5u200bu0020U000e0043u2014u058au3d0aufe57u2035u2028u2029",