a method for deformation computation based on strain tensor elements, as an alternative to the usual way of application of gradient of displacement vector, is proposed. the method computes directly the strain tensor elements from the computed/observed changes in distances and angles between the stations of a geodetic network in two epochs of observations. displacement vector which is determined...

A 2-day workshop on the geodynamic evolution of the Alpine – Carpathian orogens and the Pannonian basin, encompassing geophysics geochemistry and geology

1. Medical Physics Department, School of Medicine, Shiraz University of Medical Sciences, Shiraz, Iran 2. Ionizing and Non-ionizing Radiation Protection Research Center (INIRPRC), Shiraz University of Medical Sciences, Shiraz, Iran 3. Student Research Committee, School of Medicine, Shiraz University of Medical Sciences, Shiraz, Iran 4. Tangestan Health Network, Bushehr University of Medical Sci...

Low-temperature thermochronometry reveals regional Late Cenozoic denudation in Fiordland, New Zealand, consistent with geodynamic models showing uplift of the overriding plate during incipient subduction. The data show a northward progression of exhumation in response to northward migration of the initiation of subduction. The locus of most recent uplift coincides with a large positive Bouguer ...

Roghieh Kharaghani, Mohammad Shariati, Afsaneh Keramat, Masud Yunesian, Alireza Moghisi. Department of Midwifery, Zanjan University of Medical Sciences, Zanjan, Iran; Department of Community Medicine, Tehran University of Medical Sciences, Tehran, Iran; Institute for Environmental Research, School of Public Health, Tehran University of Medical Sciences, Tehran, Iran; Center for Health Related S...

The Zagros orogeny in Iran is associated with two successive geodynamic events during the Tertiary period, a Paleogene NE-directed regional crustal extension followed by a Miocene NW-directed regional crustal extension and a magmatic flare-up. The current study was undertaken to reanalyze previous structural work developed on the extensional Chapedony metamorphic core complex in Central Iran ex...

It is generally believed that subduction of lithospheric slabs is a major contribution to thermal heterogeneity in Earth’s entire mantle and provides a main driving force for mantle flow. Mantle structure can, on the one hand, be inferred from plate tectonic models of subduction history and geodynamic models of mantle flow. On the other hand, seismic tomography models provide important informat...

1 Student Research Committee, School of Medicine, ShirazUniversity of Medical Sciences, Shiraz 7134845794, Iran; [email protected] 2 Tangestan Health Network, Bushehr University of Medical Sciences, Bushehr 7551866897, Iran; [email protected] 3 Ionizing and Non-Ionizing Radiation Protection Research Center (INIRPRC), ShirazUniversity of Medical Sciences, Shiraz 7134845794, Iran 4 M...