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    Please use this identifier to cite or link to this item: https://irlib.pccu.edu.tw/handle/987654321/29197


    Title: Campaigned GPS on Present-Day Crustal Deformation in Northernmost Longitudinal Valley Preliminary Results, Hualien Taiwan
    Authors: Chen, Chia-Yu
    Lee, Jian-Cheng
    Chen, Yue-Gau
    Chen, Rou-Fei
    Contributors: 地質系
    Keywords: Block rotation
    Tectonic escape
    GPS
    Plate corner
    Longitudinal Valley
    Taiwan
    Date: 2014-06
    Issue Date: 2015-01-26 10:35:16 (UTC+8)
    Abstract: The Longitudinal Valley in Eastern Taiwan sits at the collision suture between the Eurasian and Philippine Sea plates. Based on repeated GPS campaigned measurements from 25 stations six times in 2007 - 2009, we characterize the surface deformation in the northernmost Longitudinal Valley where the Coastal Range of the Philippine Sea plate turns northward diving under the Eurasian plate producing two major active faults: the Milun fault and the Longitudinal Valley fault. We reconstructed a GPS velocity field and conducted strain analyses and elastic block modeling. Our results suggest a rapid clockwise rotation of 330 Myr(-1) and an eastward tectonic escape in the small Hualien City block (HUAL) area of 10 x 10 km, which is apparently detached from the regional rotating RYUK block defined by previous studies. We interpret it as being initiated locally by the northwest indentation of the Coastal Range, which pushed the HUAL block to move upward and eastward. According to our strain analyses, the HUAL block shows a significant internal elastic strain inside the Milun Tableland, the hanging wall of the Milun fault. No significant deformation was observed across the surface trace of the fault, indicating that the Milun fault is now probably locked in the near surface. The deformation in the footwall of the fault was accommodated by pure-shear strain with a major NNW-compression and a minor ENE-extension. The deformation in the hanging wall is characterized by simple-shear strain with ENE-extension in its northern part and little deformation in the southern part, separated by a little known NW-trending active fault zone (Dongmingyi fault), which needs further investigation.
    Relation: TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES 卷: 25 期: 3 頁碼: 337-357
    Appears in Collections:[Department of Geology] journal articles

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