Comments on the paper “Stratigraphy and geochronology of Quaternary marine terraces of Tasmania, Southeastern Australia: implications on neotectonism” by Jaeryul Shin, Geosciences Journal, 17, 429–443
Comments on the paper “Stratigraphy and geochronology of Quaternary marine terraces of Tasmania, Southeastern Australia: implications on neotectonism” by Jaeryul Shin, Geosciences Journal, 17, 429–443
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Jaeryul Shin 对论文“澳大利亚东南部塔斯马尼亚第四纪海洋阶地的地层学和地质年代学：对新构造运动的影响”的评论，地球科学杂志，17, 429–443
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发表时间：
2015
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通讯作者：
P. McIntosh
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作者：
P. McIntosh
Shin（2013）计算的塔斯马尼亚岛的上升速率不支持他的论文中提供的数据。所获得的OSL年龄表明，所分析的许多矿床属于末次冰期和河流成因。在塔斯马尼亚州南部玛丽安湾的沉积物上获得的OSL年龄证实了最近的研究，表明沙子是末次冰期和风成沉积，而不是海洋（末次间冰期）沉积。早先的研究者和Shin（2013）提出的塔斯马尼亚南部异常高的抬升率被忽略了。
The uplift rates calculated for Tasmania by Shin (2013) are not supported by the data presented in his paper. The OSL ages obtained indicate a Last Glacial age and fluvial origin for many of the deposits analysed. OSL ages obtained on sediments at Mary Ann Bay in southern Tasmania confirm recent research indicating a Last Glacial age and aeolian deposition of the sands rather than marine (Last Interglacial) deposition. Anomalously high uplift rates for southern Tasmania, proposed by earlier researchers and Shin (2013), are discounted.