The geology of Spain
W Gibbons, T Moreno - 2002 - books.google.com
The Society makes every effort to ensure that the scientific and production quality of its
books matches that of its journals. Since 1997, all book proposals have been refereed by …
books matches that of its journals. Since 1997, all book proposals have been refereed by …
Synsedimentary formation of ooidal ironstone: an example from the Jurassic deposits of SE central Iran
AH Rahiminejad, H Zand-Moghadam - Ore Geology Reviews, 2018 - Elsevier
The study of the upper Lower to Middle Jurassic Badamu Formation in SE of central Iran
represents the first report of Jurassic ooidal ironstone in Iran and exhibits a record of …
represents the first report of Jurassic ooidal ironstone in Iran and exhibits a record of …
Transgressive–regressive cycles and Jurassic palaeogeography of northeast Iberia
A correlation and sequence stratigraphy study of Jurassic successions has been carried out
in the main sedimentary basins of northeast Iberia, ie, Asturias, Basque-Cantabrian, and …
in the main sedimentary basins of northeast Iberia, ie, Asturias, Basque-Cantabrian, and …
The Middle–Late Jurassic forced regression and disconformity in central Portugal: eustatic, tectonic and climatic effects on a carbonate ramp system
AC Azeredo, VP Wright, MM Ramalho - Sedimentology, 2002 - Wiley Online Library
Abstract Successions across the Middle–Upper Jurassic disconformity in the Lusitanian
Basin (west‐central Portugal) are highly varied, and were probably developed on a large …
Basin (west‐central Portugal) are highly varied, and were probably developed on a large …
Cretaceous
J Martín-Chivelet, X Berástegui, I Rosales, L Vilas… - 2002 - pubs.geoscienceworld.org
Cretaceous rocks crop out extensively in the three main Alpine orogenic belts of Spain: the
Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during …
Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during …
Palaeogeography and relative sea-level history forcing eco-sedimentary contexts in Late Jurassic epicontinental shelves (Prebetic Zone, Betic Cordillera): an …
F Olóriz, M Reolid, FJ Rodríguez-Tovar - Earth-Science Reviews, 2012 - Elsevier
The analysis of macroinvertebrate and foraminiferal assemblages from Upper Jurassic
(Middle Oxfordian to Lower Kimmeridgian) epicontinental shelf deposits in the Prebetic …
(Middle Oxfordian to Lower Kimmeridgian) epicontinental shelf deposits in the Prebetic …
[PDF][PDF] Perturbation of the carbon cycle at the Middle/Late Jurassic transition: geological and geochemical evidence
G Dromart - American journal of science: devoted to the geological …, 2003 - doc.rero.ch
A compilation of new and published stratigraphic, paleontological and geochemical data is
used to detect the reciprocal influences of carbon cycling and global environmental changes …
used to detect the reciprocal influences of carbon cycling and global environmental changes …
Oxygen and carbon isotope composition of Callovian–Lower Oxfordian (Middle–Upper Jurassic) belemnite rostra from central Poland: a record of a Late Callovian …
H Wierzbowski, K Dembicz, T Praszkier - Palaeogeography …, 2009 - Elsevier
Oxygen and carbon isotope data of well-preserved and stratigraphically well-dated
belemnite rostra are presented from a Callovian–Lower Oxfordian succession of the Polish …
belemnite rostra are presented from a Callovian–Lower Oxfordian succession of the Polish …
Major palaeoenvironmental perturbation in an Early Aptian carbonate platform: Prelude of the Oceanic Anoxic Event 1a?
The Early Aptian Oceanic Anoxic Event (OAE 1a) was characterized by intensified
greenhouse climate conditions, widespread accumulation of organic deposits in open …
greenhouse climate conditions, widespread accumulation of organic deposits in open …
Palaeoenvironmental implications of ferruginous deposits related to a Middle–Upper Jurassic discontinuity (Prebetic Zone, Betic Cordillera, southern Spain)
M Reolid, I Abad, JM Martín-García - Sedimentary Geology, 2008 - Elsevier
The Middle–Upper Jurassic boundary in the westernmost Tethyan basins is marked by a
discontinuity. A thin iron crust with ferruginous ooids and pisoids and an overlying …
discontinuity. A thin iron crust with ferruginous ooids and pisoids and an overlying …