dc.contributor.author |
Doganis, Th |
en |
dc.contributor.author |
Doufexopoulou, M |
en |
dc.date.accessioned |
2014-03-01T01:06:51Z |
|
dc.date.available |
2014-03-01T01:06:51Z |
|
dc.date.issued |
1987 |
en |
dc.identifier.issn |
0264-3707 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/9627 |
|
dc.subject |
Design Criteria |
en |
dc.subject.classification |
Geochemistry & Geophysics |
en |
dc.title |
Design criteria for kinematics |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1016/0264-3707(87)90046-9 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1016/0264-3707(87)90046-9 |
en |
heal.language |
English |
en |
heal.publicationDate |
1987 |
en |
heal.abstract |
Horizontal control networks for kinematic studies may be chosen following feasible criteria which are different from those used in classic geodetic methods. The regions which may show a kinematic. behaviour over neighbouring ones, as well as the network points, can be selected after local gravity field (geoid) information, in addition to other geophysical criteria. Then the optimization of such control networks concerns deciding upon the measurements which minimize the statistical uncertainty of points supposed to ""move"". The discussion of the gravity field criteria is followed by an example in the Greek area. In two regions which are chosen under the above considerations, a second-order network design has been made. The results of this design are presented and remarks on the possibility of detecting crustal scale motions with classic geodetic methods in Greece are also made. © 1987. |
en |
heal.publisher |
PERGAMON-ELSEVIER SCIENCE LTD |
en |
heal.journalName |
Journal of Geodynamics |
en |
dc.identifier.doi |
10.1016/0264-3707(87)90046-9 |
en |
dc.identifier.isi |
ISI:A1987L325600020 |
en |
dc.identifier.volume |
8 |
en |
dc.identifier.issue |
2-4 |
en |
dc.identifier.spage |
301 |
en |
dc.identifier.epage |
312 |
en |