台灣西南部旗山斷層之磁力調查研究

盧至彥

doi:10.6844/NCKU.2010.01368

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台灣西南部旗山斷層之磁力調查研究

Magnetic Surveying of the Chishan Fault in Southwestern Taiwan

盧至彥 , Masters　　Advisor：陸喬克　　

英文 DOI： 10.6844/NCKU.2010.01368

磁場異常；殘餘強度；磁力梯度值；活動斷層；台灣地體構造； Magnetic Anomalies ； Residual Intensity ； Gradient Value ； Active Fault ； Tectonic Provinces of Taiwan

Abstract │ Reference (39) │ Times Cited (6) │ Altmetrics

Abstract 〈TOP〉

Parallel Abstract 〈TOP〉

The Chishan Fault is one of southwestern Taiwan's major faults. The project area in this study extends from the southwestern side of Chishan Township, Kaohsiung County, to the north of Yanchao Township, Kaohsiung County. The nearby Tainan and Kaohsiung areas are densely populated, and the Chishan Fault, that may control the alignment of several mud volcanoes, is considered to be an active fault. Field geological surveys of the Chishan Fault have found few exposures of the main fault plane, and prior research in Taiwan employed large-scale monitoring data. The purpose of this study is to perform a magnetic survey in the Chishan Fault area in order to gain a better understanding of the geological structure of this area and to relate the positions of surface faulting mapped by the Central Geological Survey and National Central University to those identified by this study.
    Here, the total magnetic intensity and its gradient were measured in the study area to determine the magnetic anomalies and infer the subsurface structure. This study involved two magnetic survey lines near the southern tip of Chishan Township along with surface outcrop reconnaissance. One survey line passes through the Mud Volcano Reserve, where prior research has postulated the existence of the Chishan Fault (A). The other survey line traversed a postulated fault line (Chishan Fault B) on the east side of Chungliao Mountain. We suggest that Chishan Fault A is a high angle west-dipping fault; Chishan Fault B is a vertical fault. The significance of this study is that it provides a methodology for combining total magnetic intensity and gradient data to determine the approximate dip on an active fault such as the Chishan Fault of Taiwan.

Reference ( 39 ) 〈TOP〉

Chang, C. C., and Tseng, C. L., 1999, A Geocentric Reference System in Taiwan: Survey Review, v. 35, no. 273, p. 195-203.
連結：
Chen, C. C., and Chen, C. S., 1998, Preliminary Result of Magnetotelluric Soundings in the Fold-Thrust Belt of Taiwan and Possible Detection of Dehydration, Tectonophysics, 292, p. 101-117.
連結：
Chen, S. W., 2005, Magnetic Surveying of the Chaochou Fault, Master’s Thesis, National Cheng Kung University, Department of Resources Engineering, 80 p.
連結：
Ching, K. E., Rau, R. J., Lee, J. C., and Hu, J. C., 2007, Contemporary Deformation of Tectonic Escape in SW Taiwan from GPS Observations, 1995–2005, Earth and Planetary Science Letters, 262, p. 601-619.
連結：
Chow, J. J., Chang, S. K., Yu, H. S., 2006, GPR Reflection Characteristics and Depositional Models of Mud Volcanic Sediments - Wushanting Mud Volcano Field, Southwestern Taiwan, Journal of Applied Geophysics, 60, p. 179-200.
連結：

Times Cited (6) 〈TOP〉

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