Absolute gravity change in Taiwan: Present result of geodynamic process investigation

Ricky Kao, Cheinway Hwang, Jeong Woo Kim, Kuo-En Ching, Frédéric Masson, Wen Chi Hsieh, Nicolas Le Moigne, Ching Chung Cheng

Research output: Contribution to journalArticle

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Abstract

Gravity values at 24 sites over 2004-2016 measured with absolute gravimeters are used to study geodynamic processes in Taiwan. We model rain-induced gravity effects and other temporal effects of non-geodynamic origins to obtain residual gravity, which cannot be fully explained by GPS-derived vertical displacements. We explain the gravity changes associated with deposited debris, earthquake, volcanism and Moho deepening. Gravity changes of 53.37 and 23.38 μGal near Sinwulyu and Laonong Rivers are caused by typhoon Morakot, leading to estimated volumes of 6.0 × 105 and 3.6 × 105 m3 in deposited debris. The observed co-seismic gravity change near the epicenter of the M 6.9 Pingtung earthquake (26 December 2006) is 3.12 ± 0.99 μGal, consistent with a dislocation-based gravity change at the μGal level, thereby supplying a gravity constraint on the modeled fault parameters. The AG record at the Tatun Volcano Group is the longest, but large temporal gravity effects here has led to a current gravity signal-to-noise ratio of less than one, which cannot convince a sinking magma chamber, but supply an error bound for gravity detections of long-term or transient magma movements. The gravity values at Ludao and Lanyu decline steadily at the rates of-2.20 and-0.50 μGal yr-1, consistent with the expected magma states of the two extinct volcanoes. The gravity rates at an uplifting site in central Taiwan and three subsiding sites in eastern Taiwan are negative, and are potentially caused by Moho deepening at a rate of-3.34 cm yr-1 and a combined Moho deepening and plate subduction at the rates of-0.18,-2.03, and-1.34 cm yr-1.

Original languageEnglish
JournalTerrestrial, Atmospheric and Oceanic Sciences
Volume28
Issue number6
DOIs
Publication statusPublished - 2017 Dec 1

Fingerprint

geodynamics
gravity
Moho
volcano
magma
earthquake
typhoon
earthquake epicenter
dislocation
magma chamber
signal-to-noise ratio
volcanism
subduction
GPS

All Science Journal Classification (ASJC) codes

  • Oceanography
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)

Cite this

Kao, Ricky ; Hwang, Cheinway ; Kim, Jeong Woo ; Ching, Kuo-En ; Masson, Frédéric ; Hsieh, Wen Chi ; Moigne, Nicolas Le ; Cheng, Ching Chung. / Absolute gravity change in Taiwan : Present result of geodynamic process investigation. In: Terrestrial, Atmospheric and Oceanic Sciences. 2017 ; Vol. 28, No. 6.
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abstract = "Gravity values at 24 sites over 2004-2016 measured with absolute gravimeters are used to study geodynamic processes in Taiwan. We model rain-induced gravity effects and other temporal effects of non-geodynamic origins to obtain residual gravity, which cannot be fully explained by GPS-derived vertical displacements. We explain the gravity changes associated with deposited debris, earthquake, volcanism and Moho deepening. Gravity changes of 53.37 and 23.38 μGal near Sinwulyu and Laonong Rivers are caused by typhoon Morakot, leading to estimated volumes of 6.0 × 105 and 3.6 × 105 m3 in deposited debris. The observed co-seismic gravity change near the epicenter of the M 6.9 Pingtung earthquake (26 December 2006) is 3.12 ± 0.99 μGal, consistent with a dislocation-based gravity change at the μGal level, thereby supplying a gravity constraint on the modeled fault parameters. The AG record at the Tatun Volcano Group is the longest, but large temporal gravity effects here has led to a current gravity signal-to-noise ratio of less than one, which cannot convince a sinking magma chamber, but supply an error bound for gravity detections of long-term or transient magma movements. The gravity values at Ludao and Lanyu decline steadily at the rates of-2.20 and-0.50 μGal yr-1, consistent with the expected magma states of the two extinct volcanoes. The gravity rates at an uplifting site in central Taiwan and three subsiding sites in eastern Taiwan are negative, and are potentially caused by Moho deepening at a rate of-3.34 cm yr-1 and a combined Moho deepening and plate subduction at the rates of-0.18,-2.03, and-1.34 cm yr-1.",
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Absolute gravity change in Taiwan : Present result of geodynamic process investigation. / Kao, Ricky; Hwang, Cheinway; Kim, Jeong Woo; Ching, Kuo-En; Masson, Frédéric; Hsieh, Wen Chi; Moigne, Nicolas Le; Cheng, Ching Chung.

In: Terrestrial, Atmospheric and Oceanic Sciences, Vol. 28, No. 6, 01.12.2017.

Research output: Contribution to journalArticle

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AB - Gravity values at 24 sites over 2004-2016 measured with absolute gravimeters are used to study geodynamic processes in Taiwan. We model rain-induced gravity effects and other temporal effects of non-geodynamic origins to obtain residual gravity, which cannot be fully explained by GPS-derived vertical displacements. We explain the gravity changes associated with deposited debris, earthquake, volcanism and Moho deepening. Gravity changes of 53.37 and 23.38 μGal near Sinwulyu and Laonong Rivers are caused by typhoon Morakot, leading to estimated volumes of 6.0 × 105 and 3.6 × 105 m3 in deposited debris. The observed co-seismic gravity change near the epicenter of the M 6.9 Pingtung earthquake (26 December 2006) is 3.12 ± 0.99 μGal, consistent with a dislocation-based gravity change at the μGal level, thereby supplying a gravity constraint on the modeled fault parameters. The AG record at the Tatun Volcano Group is the longest, but large temporal gravity effects here has led to a current gravity signal-to-noise ratio of less than one, which cannot convince a sinking magma chamber, but supply an error bound for gravity detections of long-term or transient magma movements. The gravity values at Ludao and Lanyu decline steadily at the rates of-2.20 and-0.50 μGal yr-1, consistent with the expected magma states of the two extinct volcanoes. The gravity rates at an uplifting site in central Taiwan and three subsiding sites in eastern Taiwan are negative, and are potentially caused by Moho deepening at a rate of-3.34 cm yr-1 and a combined Moho deepening and plate subduction at the rates of-0.18,-2.03, and-1.34 cm yr-1.

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