Results 31 to 40 of about 3,089 (207)

Mangarara Formation: exhumed remnants of a middle Miocene, temperate carbonate, submarine channel-fan system on the eastern margin of Taranaki Basin, New Zealand [PDF]

, 2009
The middle Miocene Mangarara Formation is a thin (1–60 m), laterally discontinuous unit of moderately to highly calcareous (40–90%) facies of sandy to pure limestone, bioclastic sandstone, and conglomerate that crops out in a few valleys in North ...
Armstrong BD, Betzler C, Beu AG, Gani MR, Harris D, Harris D, Hay RF, Hayward BW, Hornibrook N, Hornibrook N, Hunt D, Hunt TM, Lowe DR, Lowe DR, Martin JM, Nelson CS, Nodder SD, Piper DJW, Posamentier HW, Puga‐Bernabéu A, Reading HG, Ricketts BD, Ruíz‐Ortíz PA, Shanmugam G, Stagpoole V, Wright VP   +25 more
core   +2 more sources

The mid-Langhian flooding in the eastern Central Paratethys: integrated stratigraphic data from the Transylvanian Basin and SE Carpathian Foredeep [PDF]

International Journal of Earth Sciences, 2019
The mid-Langhian (“Badenian”) flooding fully reconnected the semi-isolated Central Paratethys realm with the Mediterranean and, thereby, drastically changed the middle Miocene paleogeography of Central Europe. Due to the scattered stratigraphic record and scarcity of independent age constraints in some areas, the precise age and underlying mechanism ...
Sant K., Palcu D. V., Turco E., Di Stefano A., Baldassini N., Kouwenhoven T., Kuiper K. F., Krijgsman W.   +7 more
openaire   +3 more sources

Chronostratigraphic ranges of Early–Middle Miocene larger benthic foraminifera calibrated by planktonic foraminiferal assemblages (Sierra de Marmolance, Granada, SE Spain) [PDF]

Journal of Micropalaeontology
An ∼ 300 m thick succession of bioclastic limestones and marls crops out in the Sierra de Marmolance (Subbetic Domain, External Zones, Betic Cordillera, SE Spain).
M. Bolivar-Feriche, J. Reolid, J. Aguirre, D. Bassi, J. C. Braga   +4 more
doaj   +1 more source

Firmground ichnofacies recording high-frequency marine flooding events (Langhian transgression, Vallés-Penedés Basin, Spain)

Geologica Acta, 2005
The decapod burrow Spongeliomorpha sudolica occurs associated with transgressive firmgrounds in the transition between Aragonian continental red beds and Langhian marine units in some of the inner sectors of the Vallès-Penedès Basin.
Jordi M. de Gibert Atienza, J.M. Robles
doaj   +1 more source

Changes in dip and frictional properties of the basal detachment controlling orogenic wedge propagation and frontal collapse: the External central Betics case [PDF]

, 2016
Thin-skinned fold-and-thrust belts (FTBs) have been extensively studied through both field examples and modelling. The overall dynamics of FTBs are, therefore, well understood. One less understood aspect is the combined influence of across-strike changes
Balanyá, JC, Díaz-Azpiroz, M, Expósito, I, Jimenez-Bonilla, A, Torvela, T   +4 more
core   +1 more source

Syn-tectonic sedimentary evolution of the Miocene Çatallar Basin, southwestern Turkey [PDF]

, 2009
International audienceThe Çatallar Basin is one of the Miocene basins located in the southern part of the Bey Dağları Massif (SW Turkey). This basin has been reinvestigated and new stratigraphic and sedimentological data are now presented.
Ciner, A., Kosun, Erdal, Monod, Olivier, Poisson, André, Wernli, Roland   +4 more
core   +3 more sources

Middle and Late Miocene palynological biozonation of the south-western part of Central Paratethys (Croatia)

Geologia Croatica, 2012
Middle and Late Miocene palynological biozonation of the south-western parts of Central Paratethys (Croatia) is presented based on organic-walled phytoplankton.
Koraljka Bakrač, Georg Koch, Jasenka Sremac   +2 more
doaj   +1 more source

Tracking sand-fairways through a deformed turbidite system : the Numidian (Miocene) of Central Sicily, Italy [PDF]

, 2017
The research presented here is funded by BG Group in partnership with CNPq-Brazil (National Council for Scientific and Technological Development). Rosanna Maniscalco acknowledges a FIR 2014 grant awarded from the University of Catania. We thank Christian
Baldassini, Niccolò, Butler, Robert W. H., Di Stefano, Agata, Hartley, Adrian J., Maniscalco, Rosanna, Pinter, Patricia R.   +5 more
core   +1 more source

A critical revision of the fossil record, stratigraphy and diversity of the Neogene seal genus Monotherium (Carnivora, Phocidae) [PDF]

, 2018
Historically, Monotherium had been one of the few genera of extinct Phocidae (true seals) that served as a wastebin taxon. Consequently, it did neither aid in understanding phylogenetic relationships of extinct Phocidae, nor in understanding seal ...
Dewaele, Leonard, Lambert, Olivier, Louwye, Stephen   +2 more
core   +2 more sources

Modavite finds in Middle Miocene (Langhian Stage) deposits of southwestern Poland

Carnets Geol, 2020
Most of the Ries tektites (moldavites) were deposited in sediments clearly postdating the Ries crater formation. This suggests secondary deposition for these ejected glasses. Only a few sedimentary formations known to contain these tektites are of Middle Miocene age and coeval with the Ries event. One is the Poznanska Formation, which is exposed across
openaire   +3 more sources