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新元古代普遍认可的冰期有凯噶斯、司图特、马林诺、噶斯奇厄斯,而在华南板块只有江口(司图特)冰期和南沱(马林诺)冰期具有明确的沉积记录.凯噶斯冰期只有同位素和化学指标的显示,表明可能存在寒冷气候和局部山岳冰川.噶斯奇厄斯冰期在华南板块则对应于陡山沱组沉积期间年龄相当的一个碳同位素负漂移,不过不说明华南板块是冰川气候.江口冰期期间华南板块无古地磁数据,因此其古地理位置不确定.凯噶斯和南沱冰期期间华南板块均处在中纬度.根据现有资料,在上述新元古代冰期期间华南板块均可能处在相似的中纬度.
Most of the Neoproterozoic glaciations include the Cretaceous, Stuart, Malinuo, and Garschyes, whereas in the South China Plateau, only the glacial stages of the Eguchi (Stuart) and the ice ages of Nantuo (Malinuo) Sedimentary records. Only the Isotopes and chemical indicators of the Chikas glaciation indicate the possible presence of cold climates and local mountain glaciers. The Garschians ice age in the South China Plate corresponds to an age-negative carbon isotope negative during the deposition of the Doushantuo Formation However, it does not indicate that the South China Plate is a glacier climate. The South China Plate during the Jiangkou Glaciation has no paleomagnetic data, so the paleogeographic location is uncertain. The South China Plate during the Sagar and Nantuo glaciations are all at mid- latitude. According to available data, The South China Plate during the Neoproterozoic ice age may be at a similar mid-latitude.