RT Journal Article
T1 La faciès Muschelkalk en la franja Mijares-Monserrat (Cordillera Ibérica Meridional, Valencia)
A1 Sánchez Fernández, D.
A1 Martín Chivelet, Javier
A1 López Gómez, José
A1 Márquez Aliaga, Ana
A1 Márquez, Leopoldo
AB The stratigraphical and sedimentological study of the Muschelkalk facies (Middle Triassic) carbonated unit in Mijares-Monserrat sector, (E. Spain), allows the recognition of subunits with different characteristics. The vertical evolution of these subunits represents the transition from alternate inter-subtidal shallow platform environments to inter-supratidal environments. Presence of the bivalves Leptochondria alberti, Bakevellia costata, Entolium discites and "Placunopsis"and the foraminifers Lamelliconus ex gr. ventroplanus-biconvexus, L. multispirus, L. procerus and Triado- discus eomesozoicus indicate a Ladinian-Carnian age in a broad sense. These general characteristics are common of the so- called "Mediterranean Triassic type" and particularly to the upper part of the carbonate unit of the Muschelkalk facies.
PB Sociedad Geológica de España
SN 1576-5172
YR 2005
FD 2005
LK https://hdl.handle.net/20.500.14352/52490
UL https://hdl.handle.net/20.500.14352/52490
LA spa
DS Docta Complutense
RD 7 may 2024