Tectonic implied results from geoid and topography signals

dc.contributor.author	Δουφεξοπούλου, Μαρία Γ.	el
dc.contributor.author	Παγούνης, Βασίλειος Ν.	el
dc.date.accessioned	2015-06-05T17:43:30Z
dc.date.available	2015-06-05T17:43:30Z
dc.date.issued	2015-06-05
dc.identifier.uri	http://hdl.handle.net/11400/15173
dc.rights	Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/us/	*
dc.source	http://www.sciencedirect.com/science/article/pii/S146418950000017X#	el
dc.subject	Lithosphere
dc.subject	Earth (Planet)--Figure
dc.subject	Global Positioning System
dc.subject	Tectonics
dc.subject	Λιθόσφαιρα
dc.subject	Γη (Πλανήτης) - Εικόνα
dc.subject	Παγκόσμιο Σύστημα Εντοπισμού Θέσης
dc.subject	Τεκτονική
dc.title	Tectonic implied results from geoid and topography signals	en
heal.type	journalArticle
heal.classification	Environmental sciences
heal.classification	Topography
heal.classification	Περιβαλλοντικές Επιστήμες
heal.classification	Τοπογραφία
heal.classificationURI	http://id.loc.gov/authorities/subjects/sh92004048
heal.classificationURI	http://skos.um.es/unescothes/C04078
heal.classificationURI	N/A-Περιβαλλοντικές Επιστήμες
heal.classificationURI	N/A-Τοπογραφία
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh2011000728
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh85040434
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh86003934
heal.keywordURI	http://skos.um.es/unesco6/250707
heal.identifier.secondary	ISSN: 14641895
heal.identifier.secondary	DOI: 10.1016/S1464-1895(00)00017-X
heal.access	campus
heal.recordProvider	Σχολή Τεχνολογικών Εφαρμογών. Τμήμα Πολιτικών Μηχανικών Τ.Ε. και Μηχανικών Τοπογραφίας και Γεωπληροφορικής Τ.Ε. Κατεύθυνση Μηχανικών Τοπογραφίας & Γεωπληροφορικής Τ.Ε.	el
heal.publicationDate	2000
heal.bibliographicCitation	Doufexopoulou, M. G. and Pagounis, V. N. (2000). Tectonic implied results from geoid and topography signals. "Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy", 25(1), 2000. pp 101-106. Available from: http://www.sciencedirect.com/science/article/pii/S146418950000017X. [Accessed 10/10/1999]	en
heal.abstract	The topographic surface is a measure of static equilibrium from the actual density distribution within the outmost Earth's lithosphere. The natural height reference of this surface, known as geoid, reflects the mixed mass-density effects, caused by the same sources, without the contribution of topographic mass. Geoid undulation and topography are output signals, which carry in common a large part of the contribution from the causal 'sources'. This contribution appears in both types of signal. Comparisons between the signals depict the geographical location and an estimation of the depth occurrence of areas with geophysical and tectonic formations depending on their correlation rate. We present results from the Greek region, known for its complex diversity in topography, tectonics and dynamics. The tests are in point and 'surface' concept, from local and global signals of geoid and topography. Local geoid is represented at 91 GPS points and EGM 96 coefficients compute its global representation. The topography is point values within the area, and the ETOPO5 5'X5' data within the geographical frame.	en
heal.publisher	Elsevier Science Ltd	en
heal.journalName	Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy	en
heal.journalType	peer-reviewed
heal.fullTextAvailability	true