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dc.contributor.authorPearson, Christopher
dc.contributor.authorManandhar, Niraj
dc.contributor.authorDenys, Paul
dc.date.available2020-03-31T23:42:48Z
dc.date.copyright2016-05
dc.identifier.citationPearson, C., Manandhar, N., & Denys, P. (2016). Towards a Modernized Geodetic Datum for Nepal: Options for Developing an Accurate Terrestrial Reference Frame Following the April 25, 2015 Mw7.8 Gorkha Earthquake. In Https://www.fig.net/resources/proceedings/fig_proceedings/fig2016/index.htm. Presented at the FIG Working Week 2016 - Recovery from Disaster, FIG.en
dc.identifier.isbn978-87-92853-52-3
dc.identifier.issn2307-4086
dc.identifier.urihttp://hdl.handle.net/10523/10003
dc.description.abstractAlong with the damage to buildings and infrastructure, the April 25, 2015 Mw7.8 Gorkha earthquake caused significant deformation over a large area of eastern Nepal with displacements of over 2 m recorded in the vicinity of Kathmandu. In this paper we consider options for a modernized geodetic datum for Nepal that will have the capacity to correct for the earthquake displacements and ongoing tectonic deformation associated with Nepal’s location on the India/Eurasian plate boundary. The current Nepal datum is a classical datum developed in 1984 by the Military Survey branch of the Royal (UK) Engineers in collaboration with the Nepal Survey Department. It has served Nepal well; however, the recent earthquakes have provided an impetus for developing a semi-dynamic datum that will be based on the most current available ITRF and have the capacity to correct for tectonic deformation. In the scenario we present here, the datum would be based on ITRF2014 with a reference epoch set some time after the end of the current sequence of earthquakes. The deformation model contains a grid of the secular velocity field combined with models of the Gorkha Earthquake and the May 12 Mw7.3 aftershock. We have developed a preliminary velocity field by collating GPS derived crustal velocities from four previous studies for Nepal and adjacent parts of China and India and aligning them to the ITRF. We are currently working on developing patches for the co-seismic part of the deformation using published dislocation models. While these models do a reasonably good job of modelling the deformation, there are some significant discrepancies between their predictions and the limited GPS measurements available. We hope to improve these models by developing revised grids that will incorporate increased GPS and INSAR measurements of the deformation field. High order control would be a CORS network based around the existing Nepal GPS Array. Coordinates for existing lower order control would be determined by readjusting existing survey measurements and these would be combined with a series of new control stations spread throughout Nepal.en_NZ
dc.format.mimetypeapplication/pdf
dc.language.isoenen_NZ
dc.publisherFIGen_NZ
dc.relation.ispartofhttps://www.fig.net/resources/proceedings/fig_proceedings/fig2016/index.htmen_NZ
dc.relation.urihttps://www.fig.net/resources/proceedings/fig_proceedings/fig2016/papers/ts01b/TS01B_pearson_manandhar_et_al_7970.pdfen_NZ
dc.subjectNational deformation models, geodetic reference systems, Nepalen_NZ
dc.titleTowards a Modernized Geodetic Datum for Nepal: Options for Developing an Accurate Terrestrial Reference Frame Following the April 25, 2015 Mw7.8 Gorkha Earthquakeen_NZ
dc.typeConference or Workshop Item (Paper)en_NZ
dc.date.updated2020-03-31T23:13:47Z
otago.schoolSchool of Surveyingen_NZ
otago.openaccessOpenen_NZ
otago.event.placeChristchurch, New Zealanden_NZ
otago.event.titleFIG Working Week 2016 - Recovery from Disasteren_NZ
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