台灣西南海岸平原環境變遷後續研究─(子計畫四)台灣西南海岸岩心沉積物之穩定硫同位素研究
Other Title
Stable Sulfur Isotope Analysis of Core Sediments in southwestern
Coast of Taiwan
Coast of Taiwan
Date Issued
1998
Date
1998
Author(s)
DOI
872116M002022
Abstract
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.
Subjects
Zaikang core
Stable sulfur isotope
Holocene transgression
Publisher
臺北市：國立臺灣大學地質科學系暨研究所
Type
report
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