即席演说
发表于 2025-3-28 15:54:15
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有特色
发表于 2025-3-28 21:53:03
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cravat
发表于 2025-3-28 23:39:26
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grudging
发表于 2025-3-29 03:27:54
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BOLUS
发表于 2025-3-29 07:34:15
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枫树
发表于 2025-3-29 11:48:29
Joachim Rösler,Harald Harders,Martin Bäkers formed, notably xenoliths in kimberlites. Outside cratonic areas where kimberlites typically occur, diamonds have been recorded in alpine peridot-ites and gravels associated with them. Graphite pseudomorphs after di-amonds occur in the Beni Bousera peridotite massif (Kornprobst, 1969) within garne
青春期
发表于 2025-3-29 18:08:14
Joachim Rösler,Harald Harders,Martin Bäkers formed, notably xenoliths in kimberlites. Outside cratonic areas where kimberlites typically occur, diamonds have been recorded in alpine peridot-ites and gravels associated with them. Graphite pseudomorphs after di-amonds occur in the Beni Bousera peridotite massif (Kornprobst, 1969) within garne
鸵鸟
发表于 2025-3-29 21:27:09
Joachim Rösler,Harald Harders,Martin Bäkers formed, notably xenoliths in kimberlites. Outside cratonic areas where kimberlites typically occur, diamonds have been recorded in alpine peridot-ites and gravels associated with them. Graphite pseudomorphs after di-amonds occur in the Beni Bousera peridotite massif (Kornprobst, 1969) within garne
Encephalitis
发表于 2025-3-30 01:43:17
Joachim Rösler,Harald Harders,Martin Bäkers formed, notably xenoliths in kimberlites. Outside cratonic areas where kimberlites typically occur, diamonds have been recorded in alpine peridot-ites and gravels associated with them. Graphite pseudomorphs after di-amonds occur in the Beni Bousera peridotite massif (Kornprobst, 1969) within garne
anesthesia
发表于 2025-3-30 06:31:40
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