OpenAccessBelV2, PascalFrancis, Corpus, bibRecord, 000167

Recent tectonic evidenced by SAR interferometry in the East African rift. ESA project AOI.b201

Identifieur interne : 000167 ( PascalFrancis/Corpus ); précédent : 000166; suivant : 000168

Recent tectonic evidenced by SAR interferometry in the East African rift. ESA project AOI.b201

Auteurs : F. Kervyn

Source :

ESA SP [ 0379-6566 ] ; 1997.

RBID : Pascal:98-0508865

Descripteurs français

Pascal (Inist)
- Malawi, Rift Est Africain, Radar antenne synthétique, Fossé, Interférométrie, Ligne directionnelle, Glissement, Carte topographique, Télédétection spatiale, Contrôle tectonique, Modèle, Relief, Satellite ERS.

English descriptors

KwdEn :
- East African Rift, Malawi, Space remote sensing, interferometry, models, relief, slip, strike, synthetic aperture radar, tectonic controls, topographic maps, troughs.

Abstract

SAR interferometry and related tools open new possibilities for geological applications in regions where field access is limited. Production of interferometric DEM with good vertical resolution offers facilities for geomorphologic interpretations. We are using such DEMs for the study of the Rukwa rift situated between the Tanganyika and Malawi tectonic troughs which is showing both highly pronounced and subtle tectonic features that the interferometry technique can evidence. The Rukwa rift is a deep NW-SE trending sedimentary basin where both normal and strike-slip movements are recorded in the recent times. Field experience has demonstrated the support of such DEMs for slight topographic features identification which are not visible on existing topographic maps. This work is taking place within a more global and pluridisciplinary study of that part of the East African rift.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A06				`@2 414 @3 p.1`
A08	`01`	`1`	`ENG`	`@1 Recent tectonic evidenced by SAR interferometry in the East African rift. ESA project AOI.b201`
A09	`01`	`1`	`ENG`	`@1 Space at the service of our environment : Florence, 14-21 March 1997`
A11	`01`	`1`		`@1 KERVYN (F.)`
A14	`01`			`@1 Royal Museum for Central Africa, 13, Leuvensesteenweg @2 3080 Tervuren @3 BEL @Z 1 aut.`
A18	`01`	`1`		`@1 European Space Agency @2 Paris @3 FRA @9 patr.`
A20				`@1 579-582`
A21				`@1 1997`
A23	`01`			`@0 ENG`
A26	`01`			`@0 92-9092-656-2`
A43	`01`			`@1 INIST @2 22484 @5 354000070122310980`
A44				`@0 0000 @1 © 1998 INIST-CNRS. All rights reserved.`
A45				`@0 6 ref.`
A47	`01`	`1`		`@0 98-0508865`
A60				`@1 P @2 C`
A61				`@0 A`
A64		`1`		`@0 ESA SP`
A66	`01`			`@0 NLD`
C01	`01`		`ENG`	@0 SAR interferometry and related tools open new possibilities for geological applications in regions where field access is limited. Production of interferometric DEM with good vertical resolution offers facilities for geomorphologic interpretations. We are using such DEMs for the study of the Rukwa rift situated between the Tanganyika and Malawi tectonic troughs which is showing both highly pronounced and subtle tectonic features that the interferometry technique can evidence. The Rukwa rift is a deep NW-SE trending sedimentary basin where both normal and strike-slip movements are recorded in the recent times. Field experience has demonstrated the support of such DEMs for slight topographic features identification which are not visible on existing topographic maps. This work is taking place within a more global and pluridisciplinary study of that part of the East African rift.
C02	`01`	`2`		`@0 225B04`
C02	`02`	`2`		`@0 225A`
C02	`03`	`X`		`@0 001E01M04`
C02	`04`	`X`		`@0 001E01L`
C03	`01`	`2`	`FRE`	`@0 Malawi @2 NG @5 01`
C03	`01`	`2`	`ENG`	`@0 Malawi @2 NG @5 01`
C03	`01`	`2`	`SPA`	`@0 Malawi @2 NG @5 01`
C03	`02`	`2`	`FRE`	`@0 Rift Est Africain @2 NG @5 02`
C03	`02`	`2`	`ENG`	`@0 East African Rift @2 NG @5 02`
C03	`02`	`2`	`SPA`	`@0 Rift Este Africano @2 NG @5 02`
C03	`03`	`2`	`FRE`	`@0 Radar antenne synthétique @5 06`
C03	`03`	`2`	`ENG`	`@0 synthetic aperture radar @5 06`
C03	`04`	`2`	`FRE`	`@0 Fossé @5 11`
C03	`04`	`2`	`ENG`	`@0 troughs @5 11`
C03	`05`	`2`	`FRE`	`@0 Interférométrie @5 12`
C03	`05`	`2`	`ENG`	`@0 interferometry @5 12`
C03	`05`	`2`	`SPA`	`@0 Interferometría @5 12`
C03	`06`	`2`	`FRE`	`@0 Ligne directionnelle @5 13`
C03	`06`	`2`	`ENG`	`@0 strike @5 13`
C03	`07`	`2`	`FRE`	`@0 Glissement @5 14`
C03	`07`	`2`	`ENG`	`@0 slip @5 14`
C03	`08`	`2`	`FRE`	`@0 Carte topographique @5 16`
C03	`08`	`2`	`ENG`	`@0 topographic maps @5 16`
C03	`08`	`2`	`SPA`	`@0 Plano topográfico @5 16`
C03	`09`	`2`	`FRE`	`@0 Télédétection spatiale @5 19`
C03	`09`	`2`	`ENG`	`@0 Space remote sensing @5 19`
C03	`09`	`2`	`SPA`	`@0 Teledetección espacial @5 19`
C03	`10`	`2`	`FRE`	`@0 Contrôle tectonique @5 20`
C03	`10`	`2`	`ENG`	`@0 tectonic controls @5 20`
C03	`10`	`2`	`SPA`	`@0 Control tectónico @5 20`
C03	`11`	`2`	`FRE`	`@0 Modèle @5 23`
C03	`11`	`2`	`ENG`	`@0 models @5 23`
C03	`11`	`2`	`SPA`	`@0 Modelo @5 23`
C03	`12`	`2`	`FRE`	`@0 Relief @5 24`
C03	`12`	`2`	`ENG`	`@0 relief @5 24`
C03	`13`	`2`	`FRE`	`@0 Satellite ERS @4 INC @5 52`
C06				`@0 ILS`
C07	`01`	`2`	`FRE`	`@0 Afrique Est @2 NG`
C07	`01`	`2`	`ENG`	`@0 East Africa @2 NG`
C07	`01`	`2`	`SPA`	`@0 Africa oriental @2 NG`
C07	`02`	`2`	`FRE`	`@0 Afrique`
C07	`02`	`2`	`ENG`	`@0 Africa`
C07	`02`	`2`	`SPA`	`@0 Africa`
N21				`@1 334`

A30	`01`	`1`	`ENG`	`@1 ERS symposium on space at the service of our environment @2 3 @3 Florence ITA @4 1997-03-14`

Format Inist (serveur)

NO :	PASCAL 98-0508865 INIST
ET :	Recent tectonic evidenced by SAR interferometry in the East African rift. ESA project AOI.b201
AU :	KERVYN (F.)
AF :	Royal Museum for Central Africa, 13, Leuvensesteenweg/3080 Tervuren/Belgique (1 aut.)
DT :	Publication en série; Congrès; Niveau analytique
SO :	ESA SP; ISSN 0379-6566; Pays-Bas; Da. 1997; No. 414 p.1; Pp. 579-582; Bibl. 6 ref.
LA :	Anglais
EA :	SAR interferometry and related tools open new possibilities for geological applications in regions where field access is limited. Production of interferometric DEM with good vertical resolution offers facilities for geomorphologic interpretations. We are using such DEMs for the study of the Rukwa rift situated between the Tanganyika and Malawi tectonic troughs which is showing both highly pronounced and subtle tectonic features that the interferometry technique can evidence. The Rukwa rift is a deep NW-SE trending sedimentary basin where both normal and strike-slip movements are recorded in the recent times. Field experience has demonstrated the support of such DEMs for slight topographic features identification which are not visible on existing topographic maps. This work is taking place within a more global and pluridisciplinary study of that part of the East African rift.
CC :	225B04; 225A; 001E01M04; 001E01L
FD :	Malawi; Rift Est Africain; Radar antenne synthétique; Fossé; Interférométrie; Ligne directionnelle; Glissement; Carte topographique; Télédétection spatiale; Contrôle tectonique; Modèle; Relief; Satellite ERS
FG :	Afrique Est; Afrique
ED :	Malawi; East African Rift; synthetic aperture radar; troughs; interferometry; strike; slip; topographic maps; Space remote sensing; tectonic controls; models; relief
EG :	East Africa; Africa
SD :	Malawi; Rift Este Africano; Interferometría; Plano topográfico; Teledetección espacial; Control tectónico; Modelo
LO :	INIST-22484.354000070122310980
ID :	98-0508865

Links to Exploration step

Pascal:98-0508865

Le document en format XML

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<ET>Recent tectonic evidenced by SAR interferometry in the East African rift. ESA project AOI.b201</ET>
<AU>KERVYN (F.)</AU>
<AF>Royal Museum for Central Africa, 13, Leuvensesteenweg/3080 Tervuren/Belgique (1 aut.)</AF>
<DT>Publication en série; Congrès; Niveau analytique</DT>
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   |clé=     Pascal:98-0508865
   |texte=   Recent tectonic evidenced by SAR interferometry in the East African rift. ESA project AOI.b201
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	Serveur d'exploration autour du libre accès en Belgique
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Recent tectonic evidenced by SAR interferometry in the East African rift. ESA project AOI.b201

Recent tectonic evidenced by SAR interferometry in the East African rift. ESA project AOI.b201

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