作者: GERMAN MÜLLER
关键词:
摘要: IN Lake Balaton, Hungary, large quantities of fine grained, high-magnesian calcite are precipitated during the warmer seasons by a strong growth phytoplankton1,2. The formation instead “normal” (that is, low-magnesian) can be related to high Mg/Ca ratio lake water which varies locally between about one and three. electrolyte concentration is less than 500 mg/1.