作者: Mordehai Magaritz
DOI: 10.1016/0012-821X(73)90205-7
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摘要: Secondary calcites from Mount Hermon, Israel can be separated into two based on their carbon and oxygen composition. The first group has the usual isotopic composition of secondary which are precipitated waters having recent groundwaters in region. second is characterized by high 13 C low 18 O values, compared with group. European Alps show compositions similar to this A model formation these precipitation snowmelt presented, explains anomalous calcite.