Tectonic implied results from geoid and topography signals

Doufexopoulou, M; Pagounis, VN

dc.contributor.author	Doufexopoulou, M	en
dc.contributor.author	Pagounis, VN	en
dc.date.accessioned	2014-03-01T01:50:29Z
dc.date.available	2014-03-01T01:50:29Z
dc.date.issued	2000	en
dc.identifier.issn	1464-1895	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/26034
dc.subject.classification	Geochemistry & Geophysics	en
dc.title	Tectonic implied results from geoid and topography signals	en
heal.type	journalArticle	en
heal.language	English	en
heal.publicationDate	2000	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. (C) 2000 Elsevier Science Ltd. All rights reserved.	en
heal.publisher	PERGAMON-ELSEVIER SCIENCE LTD	en
heal.journalName	PHYSICS AND CHEMISTRY OF THE EARTH PART A-SOLID EARTH AND GEODESY	en
dc.identifier.isi	ISI:000086062100016	en
dc.identifier.volume	25	en
dc.identifier.issue	1	en
dc.identifier.spage	101	en
dc.identifier.epage	106	en