陳于高2006-07-252018-06-282006-07-252018-06-281998http://ntur.lib.ntu.edu.tw//handle/246246/11709本研究分析了宅港岩心中沈積物之穩 定硫同位素，其結果說明了全新世海進期 間，宅港地區雖然有海水入侵，但其環境 不若三寮灣地區穩定。至於晚更新世Stage 2 之前，宅港地區可發現兩次明顯的海進事件，此結果與三寮灣之結果類似，不過其發生的確實時間，仍有待進一步的確定。 本研究的結果，證明了硫同位素的分析，可以提供時間軸與空間軸上，環境變化的高解析度資訊。This study sequentially carried out the stable sulfur isotopic analyses of sediments in Zaikang core. The result indicates that this area was inundated during the Holocene transgression. However, the sedimentary environment was not as stable as found in the San-liao-wan core. Two significant trans-gression signals can be distinguished in the lower core, which is identified as the deposits developed earlier than Stage 2. The accurate timing of these events need to be further dated. This study confirms that the sulfur isotope analysis is able to provide the high-resolution information on not only the temporal but spatial axis.application/pdf34092 bytesapplication/pdfzh-TW國立臺灣大學地質科學系暨研究所宅港岩心穩定硫同位素全新世海進期Zaikang coreStable sulfur isotopeHolocene transgressionreporthttp://ntur.lib.ntu.edu.tw/bitstream/246246/11709/1/872116M002022.pdf