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Start Over Rights policy:public Subject 7 Subject Španělsko

1. Die Reise Kaiser Maximilian II. nach Spanien im Jahre 1548

Creator:
Ferdinand Menčík
Publisher:
C. Gerold
Format:
print, text, regular print, and 16 s. ; 25 cm
Type:
text, volume, biography, přehledy, model:monograph, and TEXT
Subject:
Geografie jako věda. Výzkum. Cestování, II., římskoněmecký císař, Maxmilián, 1527-1576, 16. století, 1548, panovníci, Svatá říše římská, cesty a pobyt, Španělsko, náklady, 929.731, 910.4, 338.58, (460), (430), (048.8), 929 Maxmilián II., 7, and 91
Language:
German
Description:
mitgetheilt von Ferdinand Menčík
Rights:
http://creativecommons.org/publicdomain/mark/1.0/ and policy:public

2. Monitoring of active tectonic structures in central Betic Cordillera (southern Spain)

Creator:
Galindo-Zaldívar, Jesús, Gil, Antonio, Sanz de Galdeano, Carlos, Shanov, Stefan, and Stanica, Dumitru
Format:
print, bez média, and svazek
Type:
article, články, model:article, and TEXT
Subject:
Geologie. Meteorologie. Klimatologie, GPS sítě, GPS netwoks, Španělsko, Spain, crustal structure, active faults, fault and fold interaction, Betic Cordillera, 7, and 551
Language:
English
Description:
The Betic Cordillera, located at the westernmost end of the Mediterranean alpine belt, is deformed by overprinted folds and faults that produced the present-day relief since the Tortonian. In the frame of the COST 625 action, four sectors have been studied in the central part of the cordillera. In the Granad a Depression, the large NW-SE Padul normal fault deforms the SW periclinal end of the Sierra Nevada antiform. MT surveys in dicate the continuity in depth of high and low angle normal seismogenic faults and the presence of act ive detachment faults. In Tabernas regi on a good example of interaction between a N W-SE propagating normal fault, E-W strike-slip faults and the fold system is studied. In the Sierra Tejeda-Zafarraya and in the Balanegra-Sierra de Gádor areas, two new GPS networks ha ve been installed to determine the interaction and the development of large antiformal struct ures and normal faults with E-W and NW-SE orientations. However, taking into account the low tectonic activity of the studi ed region, a period of more than 5 year could be needed to determine with enough accuracy the development rate of the structures., Jesús Galindo-Zaldívar, Antonio Gil, Carlos Sanz de Galdeano, Stefan Shanov and Dumitru Stanica., and Obsahuje bibliografické odkazy
Rights:
http://creativecommons.org/licenses/by-nc-sa/4.0/ and policy:public