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<datestamp>2018-01-11</datestamp>
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<title lang=en>Expected temporal absolute gravity change across the Taiwanese Orogen, a modeling approach</title>
<creator>Mouyen, M.</creator>
<creator>Masson, F.</creator>
<creator>Hwang, C.</creator>
<creator>Cheng, C. -C.</creator>
<creator>Cattin, Rodolphe</creator>
<creator>Lee, C. W.</creator>
<creator>Le Moigne, Nicolas</creator>
<creator>Hinderer, J.</creator>
<creator>Malavieille, Jacques</creator>
<creator>Bayer, Roger</creator>
<creator>Luck, B.</creator>
<contributor>Institut de physique du globe de Strasbourg (IPGS) ; Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Department of Civil Engineering [Hsinchu] ; National Chiao Tung University (NCTU)</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Center for Measurement Standards ; Industrial Technology Research Institute [Hsinchu]</contributor>
<description>International audience</description>
<source>ISSN: 0264-3707</source>
<source>Journal of Geodynamics</source>
<publisher>Elsevier</publisher>
<identifier>hal-00456035</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00456035</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00456035</source>
<source>Journal of Geodynamics, Elsevier, 2009, 48 (3-5), pp.284-291. 〈10.1016/j.jog.2009.09.004〉</source>
<identifier>DOI : 10.1016/j.jog.2009.09.004</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jog.2009.09.004</relation>
<language>en</language>
<subject lang=en>Taiwan</subject>
<subject lang=en>Gravity</subject>
<subject lang=en>Modeling</subject>
<subject lang=en>Surrection</subject>
<subject lang=en>Mass transfers</subject>
<subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject>
<subject>[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The island of Taiwan is located on the convergent boundary between the Philippine Sea plate and the Chinese continental margin. It offers very active mountain building and collapsing processes well illustrated by the rugged topography, rapid uplift and denudation, young tectonic landforms, active faulting and numerous earthquakes. In this paper, using simple models, we have estimated vertical movements and associated absolute gravity variations which can be expected along a profile crossing the southern part of the island and probably suffering the highest rates of rising. The two different tectonic styles proposed for the island, thin-skinned and thick-skinned, were taken into account. Horizontal and vertical movements were modeled by an elastic deformation code. Gravity variations due to these deformations are then modeled at a second step. They are dominated by plate and free-air effects, i.e. elevation of the topography, with several mu Gal yr(-1). By comparison, gravity changes generated by mass transfers are weak: maximum 0.1 mu Gal yr(-1) with the thin-skinned tectonic and 0.3 mu Gal yr(-1) with the thick-skinned tectonic. Though elastic rheology has limitations, this modeling offers interesting results on what gravity signal can be expected from the AGTO project (Absolute Gravity in the Taiwanese Orogen), which proposes to study the dynamic of these mountain ranges using absolute gravimetry (AG) and also including relative gravimetry (RG) and GPS measurements.</description>
<date>2009</date>
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