梅山斷層區域磁力普測 Magnetic surveys in the Meishan Fault region 黃亦璿 國立中正大學地環系
蔡旻倩, 2013
蔡旻倩, 2013
B N S
AA’
AA’
CC’
E N S 0.01SI
E 0.01SI
Mouthereau, M. et al.,2002
Mouthereau, M. et al.,2002
Mouthereau, M. et al.,2002
Mouthereau, M. et al.,2002
Tertiary basins Paleogene(古第三紀) Neogene(新第三紀)
(Lacombe, et al., 2002)
Chen et al., 2003
中新世-Aquitanian 中新世-Burdigalian 大寮層 石底層 Shaw, 1996
何春蓀, 1997
尖石期 Lin, 2001
角板山期 Lin, 2001
Lin et al., 2003
同張裂期層序 Huang et al., 2012
何春蓀, 1997
陳勉銘 粗坑層凝灰岩由火山岩岩屑、礦物顆粒、沈積岩岩屑所組成,以火山碎屑佔絕大部份,粒徑由十公分以內的火山礫至火山灰皆有。凝灰岩中的礦物主要為鐵鎂礦物、斜長石與石英,但鐵鎂礦物常被後期的碳酸鹽類礦物所取代。
蔡旻倩, 2013
Chen et al., 2008
黃姝琳,2009
黃姝琳,2009
黃姝琳,2009
The high Vp/Vs may indicate a fracture zone and may reflect the existence of fluids.(Wu et al., 2007)
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