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Non一oceanic origin of waters in the Serpentinization of Some Uitramafic Rocks from China一一D/H and 18O/16O of Waters in Serpentinites
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    Abstract:

    Hydrogen and oxygen isotopic.compositions were measured on some (L- C) serpentinite samples of ultramafic rocks from Hegenshan,Jingyu,Dong- qiao, Luobusha in China: δD=-101—-146, δ(18)O=1.0—7.55. Estimates of the isotopic compositions of waters, that produced the serpentinization of ultramafic rocks in the present work range:δD=-77—-122, δ(18)O=1.4-4.9 at 330℃. According to difference of isotopic compositions

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杨凤英,康志勤,戎合,1992,我国主要超镁铁岩蛇纹石化水的非大洋成因——(L-C)蛇纹岩的D/H和(18)O/(16)O[J].岩石矿物学杂志,11(2):111~119. Yang Fengying, Kang Zhiqin, Rong He Institute of Geology, CAGS, Beijing ,1992,Non一oceanic origin of waters in the Serpentinization of Some Uitramafic Rocks from China一一D/H and 18O/16O of Waters in Serpentinites[J]. Acta Petrologica et Mineralogica,11(2):111~119.

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