Carbon recycled into deep Earth: Evidence from dolomite dissociation in subduction-zone rocks: Comment and Reply: REPLY
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[1] Yongfeng Zhu,et al. Carbon recycled into deep Earth: Evidence from dolomite dissociation in subduction-zone rocks , 2002 .
[2] Yongfeng Zhu,et al. Phlogopite and Coesite Exsolution from Super-Silicic Clinopyroxene , 2002 .
[3] Wenbo Jiang,et al. Ultrahigh-pressure metamorphism in western Tianshan, China: Part I. Evidence from inclusions of coesite pseudomorphs in garnet and from quartz exsolution lamellae in omphacite in eclogites , 2002 .
[4] Yongfeng Zhu,et al. The mineralogy of the Kokchetav ‘lamproite’: implications for the magma evolution , 2002 .
[5] T. Kikegawa,et al. In situ X-ray observation of the reaction dolomite = aragonite + magnesite at 900–1300 K , 2002 .
[6] Wenbo Jiang,et al. Ultra-high pressure metamorphism in western Tianshan, China: Part II. Evidence from magnesite in eclogite , 2002 .
[7] R. Luth. Experimental determination of the reaction aragonite + magnesite = dolomite at 5 to 9 GPa , 2001 .
[8] T. Katsura,et al. Experimental investigation on dolomite dissociation into aragonite+magnesite up to 8.5 GPa , 2001 .
[9] Masahito Ohta,et al. Diamond‐bearing and diamond‐free metacarbonate rocks from Kumdy–Kol in the Kokchetav Massif, northern Kazakhstan , 2000 .