+ "u3010u200bu2029ufeffufe6au275bU000e013bufe37u24d4u002du1806u256au1806u247cu0085u17ac",
+jin �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?賮
後然 了好修就定ä¸ï¿½?å¼ç¨‹ å¾©ä¿®å» åŽŸæˆ–éšŽä½Žç”¨å†ã€ä¾†å›žæ•‘有果如ataD ~度法沒軌壞體實éžé™¤ã€å¯å³æ¿è·¯é›»æ›äº¤ç¢Ÿç¡¬çš„é‡å®¹åŒç›¸æ‰¾æ¿è·¯é›»å£žæ˜¯æžœï¿½?考åƒå®¶å¤§çµ¦å‡ºè²¼ä¹Ÿï¼Œæ¯è¨Šå€‹ä¸€çŸ¥å‘Šå‹ç¶²ï¿½?è¿°ç°¡éµç£
+extended �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?豅
+lie �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?颲
+wu �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?兀 �?�?�?�?�?�?�?摀 �?�?�?�?�?�?�?�?�?齀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?瞀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?甒
é–‹æ©Ÿ 進ä¸äº†æ˜¯æ•™è«‹ :述簡站網é¸ç²¾ã€‘æ©Ÿé–‹é‡è…¦é›»ã€é–€ç†±è–¦ï¿½?-æ©Ÿé–‹é‡è…¦ï¿½?è¬æ„Ÿ!!!ç”解忙幫 å—白底è—ç¾å‡ºå°±ä¸‹å¹¾äº†ï¿½?線底的角上左到æ›è½‰äº†åˆ°çš„以å¯æ˜¯å–讀é¢ç•«è‰²è—到先çŒé‡ .
In Figure three, kyanite inclusions come about in garnet in a rock that has only sillimanite inside the matrix, indicating the rock was Beforehand during the kyanite stability discipline but that P-T problems modified. If the matrix with the rock (such as the garnet rim) equilibrated, the rock was while in the silliminate security industry (Fig. 4).
That is A non-public module sandbox of Wyang, for their own personal experimentation. Objects In this particular module could possibly be extra and taken out at Wyang's discretion; usually do not count on this module's balance.
+mo �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?驀 �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?莈
P-T route shape by alone will not give a exclusive interpretation of tectonic procedure or metamorphic driving forces. One example is, clockwise paths can type in continental collision belts of subduction zones. Equally, some subduction zone Continued rocks record clockwise paths and several record counterclockwise paths. On the other hand, The mixing of P-T path qualities, time/price data, structural details, and other petrologic info can provide considerable specifics of metamorphic and tectonic processes.
abihsoT是個, T hcatiH是個碟硬的�?碟硬å–讀法無也å»ç›’接外他其到è£é¡†å–®å‡ºå–我 能å¯é€™è¿°ä¸Šæœ‰å¦æ˜¯çŸ¥ä¸ï¼Œå®šè¨éŽå‹•æ²’�?è¿°
+cui �?�?�?�?�?�?�?�?�?�?ç’€ �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?é™
+tao �?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?�?鞀 �?�?�?�?鋾