Zobrazeno 1 - 10
of 98
pro vyhledávání: '"B. C. Burchfiel"'
Autor:
R. Nakov, B. C. Burchfiel
Publikováno v:
Geosphere. 11:463-490
The generally east-west–trending Balkan orogen (eastern Europe) consists of a northern belt of folded and thrusted Mesozoic and Cenozoic strata that forms the external fold-thrust belt of late Mesozoic and early Cenozoic age, and a southern belt th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f5beb05dcee1d2a0d352040966aca78
https://doi.org/10.1130/ges01020.1
https://doi.org/10.1130/ges01020.1
Publikováno v:
Lithosphere
The Longmen Shan, located at the boundary between the Tibetan Plateau and the Sichuan Basin, has received considerable attention following the 2008 Wenchuan earthquake. However, the tectonic history of the southwestern segment of the range has remain
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::21e1ffab717ba97774b157aec1b22ca9
https://doi.org/10.1130/l263.1
https://doi.org/10.1130/l263.1
Publikováno v:
Tectonophysics. 413:127-145
Global Positioning System (GPS) data acquired between 1996 and 2004 and fault plane solutions for four seismic zones are analyzed to obtain the velocity and strain rate fields for western Bulgaria. The GPS derived velocities suggest that southwestern
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f4f0a0e9447c7dc9201dfb0573867bfd
https://doi.org/10.1016/j.tecto.2005.10.040
https://doi.org/10.1016/j.tecto.2005.10.040
Publikováno v:
Tectonophysics. 375:61-76
The ENE-tilted Mesta half-graben contains a ∼3-km-thick section of Priabonian (Late Eocene) to Oligocene sedimentary and volcanic rocks that rest unconformably on basement metamorphic rocks along its west side. Basal strata dip 50–60° E and dip
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::646e40fe88d665271389b8e75141c124
https://doi.org/10.1016/j.tecto.2003.09.001
https://doi.org/10.1016/j.tecto.2003.09.001
Publikováno v:
Journal of Geodynamics. 31:189-200
To determine the present day kinematics of the major tectonic elements in Bulgaria, part of the northern extent of the Aegean extensional system, we established and surveyed a regional GPS network in 1996, 1997 and 1998. Based on our estimates of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::80f28a83695408f98a773ef9cd6c01be
https://doi.org/10.1016/s0264-3707(00)00027-2
https://doi.org/10.1016/s0264-3707(00)00027-2
Autor:
B. C. Burchfiel
Publikováno v:
Geological Magazine. 138:219-232
This book focuses on the Tertiary extensional basins within the Alpine orogen and contains contributions from the European Commission Integrated Basin Studies Project (1992–1995), and papers from a conference with the same title as the book held in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ccffd30bcd2e0a64449008a3b50b3158
https://doi.org/10.1017/s0016756801254958
https://doi.org/10.1017/s0016756801254958
Autor:
J. Zhao, E. Wang, Zhiliang Chen, B. C. Burchfiel, Y. Liu, Leigh H. Royden, Robert W. King, X. Zhang, W. Tang
Publikováno v:
Journal of Geophysical Research: Solid Earth. 105:16215-16227
We present and interpret Global Positioning System (GPS) measurements of crustal motions for the period 1991–1998 for a network encompassing the eastern part of the Tibetan Plateau and its foreland. Relative to a Eurasian frame defined by minimizin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b25ffb52b50b41b72f2b957a6b51c0a1
https://doi.org/10.1029/2000jb900092
https://doi.org/10.1029/2000jb900092
Publikováno v:
The Journal of Geology. 107:623-631
A new map and cross sections of the Khula Kangri and Kankar Punzum–Monlakarchung High Himalayan ranges in the Tibet‐Bhutan frontier area are presented from integration of unpublished mapping from the summit section of Khula Kangri and new remote
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::776b8c3e9cb3c23e42b48d41c0072e7d
https://doi.org/10.1086/314366
https://doi.org/10.1086/314366