- About
-
The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
provided by the
Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
Search results
Showing 11 to 17 of 17 (0.018 seconds)Spelling suggestions: "subject:"erdkruste"" "subject:"kruste""
| 11 |
On the relation of stress and deformation fields to natural and induced seismicity /Bohnhoff, Marco. January 1900 (has links)
Thesis (Habilitationsschrift)--Ruhr-Universität Bochum, 2005. / "February 2006"--P. [2] of cover. Includes bibliographical references. Also available via the World Wide Web.
|
| 12 |
Elektromagnetische Arraymessungen im Rheinischen Schiefergebirge Modelle der elektrischen Leitfähigkeit der Erdkruste und des oberen Mantels mit Verbindungen zum Eifelvulkanismus /Leibecker, Jörg. Unknown Date (has links) (PDF)
Universiẗat, Diss., 2000--Göttingen.
|
| 13 |
A receiver function study of the crust and upper mantle across the dead sea transformMohsen, Ayman. Unknown Date (has links)
Freie Universiẗat, Diss., 2004--Berlin. / Dateiformat: zip, Dateien im PDF-Format.
|
| 14 |
Eine Milliarde Jahre geologischer Entwicklung am NW-Rand des Kalahari KratonsNagel, Rudolf 02 November 1999 (has links)
No description available.
|
| 15 |
Microseismic event location and passive seismic imaging of crustal structuresHassani, Hossein 08 August 2019 (has links)
This research is aimed to develop a migration-based earthquake location algorithm and a passive seismic imaging approach to investigate microseismicity and image steep crustal structures in the mining area Schlema-Alberoda. The dataset includes single-component records of several microseismic events which occurred between 1998 and 2012 in the area. Through some tests and comparisons, the accuracy of the localization algorithm is proved. An expected extension of pre-existing faults within the granitic body and the connection between some of the structures is comfirmed by the location results. The passive imaging procedure is conducted using only P-wave secondary arrivals from the relocated events and by applying 3-D coherency migration. The reliability of the passive imaging results is verified by comparing the final image with the results of a 3-D active reflection seismic survey in the same area. In addition, the passive image complements the 3-D active image and reveals new structures that have not been imaged previously.
|
| 16 |
The Geomorphic Response of the Passive Continental Margin of Northern Namibia to Gondwana Break-Up and Global Scale TectonicsRaab, Matthias Johannes 21 June 2001 (has links)
No description available.
|
| 17 |
The emplacement of the Chinamora Batholith (Zimbabwe) inferred from field observations, magnetic- and microfabricsBecker, Jens Karl 23 June 2000 (has links)
No description available.
|
Page generated in 0.0286 seconds