Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Luc-Emmanuel Ricou"'
Autor:
Jansa, Lubomir F.
Publikováno v:
PALAIOS, 1997 Oct 01. 12(5), 499-500.
Externí odkaz:
https://www.jstor.org/stable/3515389
''A voluminous encyclopedia of Tethyan geology and, as such, it provides an invaluable source of information for those interested in this region, and Earth history in general...The book is a must for the libraries of universities and geologic institu
Autor:
Hervé Bellon, Mossaı̈eb Sabzehei, Thierry Juteau, Hubert Whitechurch, Luc-Emmanuel Ricou, Habibollah Ghasemi
Publikováno v:
Comptes Rendus Geoscience. 334:431-438
The mafic–ultramafic complex of Sikhoran presents a long geological history, marked out by various magmatic, metamorphic and tectonic events. This history is much more complex than a simple ophiolite obduction over a continental margin. As early as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a90d7c3ab2ce7822d3670d3506d71e33
https://doi.org/10.1016/s1631-0713(02)01770-4
https://doi.org/10.1016/s1631-0713(02)01770-4
Autor:
Hervé Bellon, Hubert Whitechurch, Ali Kananian, Luc-Emmanuel Ricou, Ali Darvishzadeh, Mossaieb Sabzehi, Thierry Juteau
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 332:543-552
The ophiolitic massif of Kahnuj (600 km2) consists, from bottom to top, of layered gabbros, isotropic gabbros and ouralite gabbros, agmatites of dioritic to plagiogranitic composition, a sheeted dyke complex and lastly a basaltic pillow lava unit. Am
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3fdd5384bcf8ca720a687be4a3627973
https://doi.org/10.1016/s1251-8050(01)01574-9
https://doi.org/10.1016/s1251-8050(01)01574-9
Publikováno v:
Geodinamica Acta. 11:285-309
The Rhodope massif of Bulgaria and Greece is a complex of Mesozoic synmetamorphic nappes stacked in an Alpine active margin environment. A new analysis of the Triassic to Eocene history of the Vardar suture zone m Greece discloses its Cretaceous sett
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c0c924a9487a128543c9da70f51bbdbd
https://doi.org/10.1016/s0985-3111(99)80018-7
https://doi.org/10.1016/s0985-3111(99)80018-7
Autor:
Dominique Gibert, Luc-Emmanuel Ricou
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 325:753-759
The wavelet analysis of the magnetic reversal sequence since 160 Ma discloses abrupt discontinuities in the evolution of the reversal frequency. They correspond, with a mean 3 Ma delay, to major plate reorganisations as defined by the formation or de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b5203e63c645bf77dfbb910dfc357276
https://doi.org/10.1016/s1251-8050(97)82752-8
https://doi.org/10.1016/s1251-8050(97)82752-8
Publikováno v:
Geodinamica Acta. 10:189-208
Subsidence analysis is used here to get a better understanding of the Eo-Cimmerian continental accretion to Eurasia of a block (the Iran Block) of Gondwanian origin. The drift of the block from Gondwana to Eurasia is classically considered as a late
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::666ab8f774f75118e7364b0e166ec9ba
https://doi.org/10.1080/09853111.1997.11105302
https://doi.org/10.1080/09853111.1997.11105302
Publikováno v:
Earth and Planetary Science Letters. 148:553-567
The Pangea configuration for the interval of Late Carboniferous to Early Jurassic is still debated: was it similar to the well known Wegenerian Pangea or did Gondwanaland move with respect to Laurussia along a major right-lateral lineament of several
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8bf3d692b4d2dbc124341edb1413438e
https://doi.org/10.1016/s0012-821x(97)00047-2
https://doi.org/10.1016/s0012-821x(97)00047-2
Publikováno v:
Scopus-Elsevier
Mylonitic gneisses of the Bulgarian and Greek Rhodope were deformed under medium pressure-type metamorphism. The kinematic information contained in these gneisses shows that shear-deformation occurred during development of a nappe complex. Lithologie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9097c5e3520639ac50d16d697fe146d6
https://doi.org/10.1111/j.1365-3121.1996.tb00720.x
https://doi.org/10.1111/j.1365-3121.1996.tb00720.x
Autor:
Luc Emmanuel Ricou
Publikováno v:
Physics of the Earth and Planetary Interiors. 87:255-265
Using a recent step-by-step reconstruction of the Mesozoic Tethys Ocean and surrounding continents, we draw the topologic patterns which characterise the networks of plate boundaries for pre-Tethys, Tethys and post-Tethys times. We define an asymmetr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcc8ea84562259e00b8f66b8fd27c2b0
https://doi.org/10.1016/0031-9201(94)02964-d
https://doi.org/10.1016/0031-9201(94)02964-d