Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Luc-Emmanuel Ricou"'
''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
Autor:
Luc-Emmanuel Ricou
Publikováno v:
Geodinamica Acta. 7:169-218
This paper describes the evolution of the former Tethys ocean in terms of successive positions of the involved plates, their boundaries, and the oceanic and continental elements they bore. Most of the past positions for the major continents are obtai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3235ecea7ad7e09a59400e14fac337d1
https://doi.org/10.1080/09853111.1994.11105266
https://doi.org/10.1080/09853111.1994.11105266