This study reports on ooid diversity from different lithotypes of the Yacoraite Formation (Salta Group basin) in the Central Andes of north-west Argentina. The ooids display a variety of internal and external morphologies that may be deployed as proxies for seawater chemistry and hydrodynamic processes. A short review of nomenclature problems is first discussed, followed by presentation of a two-fold quantitative and qualitative methodology. Our proposed classification addresses internal and external ooid characters in order to understand growth in response to various environmental processes at an individual particle level. This classification allows discrimination between a variety of morphologies, but also evaluation of the complexity of ...
Ooids are a common type of carbonate sand grain that form through a combination of constructive and ...
Ocean Anoxic Events (OAEs) are major carbon cycle perturbations that occurred several times in the M...
The Carmel Formation formed in a shallow inland sea during the Middle Jurassic and is located in par...
The succession in the Tizra Formation shows an excellent exposure of a small open marine platform wh...
Ooids are a common component of carbonate successions of all ages and present significant potential ...
Ooids are typically found in frequently reworked coastal sediments, and are thought to accrete by in...
Ooids (subspherical particles with a laminated cortex growing around a nucleus) are ubiquitous in th...
While ooids have been significant components of many shallow-water carbonates throughout Earth’s his...
The shallow carbonate facies at the top of the Yacoraite Formation (Late Cretaceous–Early Palaeocene...
The architecture of lacustrine systems is the result of the complex interaction between tectonics, c...
Due to the complex nature and importance of porosity in carbonate systems, it has been extensively s...
Ooids, pisoids, nodules, concretions, and a host of other terms are used to describe concentrically-...
743-758This study is an attempt to describe the distribution and fabric of the Cambrian ooids from t...
International audienceIn this study, an integrated approach was applied using available sedimentary,...
In this study, an integrated approach was applied using available sedimentary, geochronology, geoche...
Ooids are a common type of carbonate sand grain that form through a combination of constructive and ...
Ocean Anoxic Events (OAEs) are major carbon cycle perturbations that occurred several times in the M...
The Carmel Formation formed in a shallow inland sea during the Middle Jurassic and is located in par...
The succession in the Tizra Formation shows an excellent exposure of a small open marine platform wh...
Ooids are a common component of carbonate successions of all ages and present significant potential ...
Ooids are typically found in frequently reworked coastal sediments, and are thought to accrete by in...
Ooids (subspherical particles with a laminated cortex growing around a nucleus) are ubiquitous in th...
While ooids have been significant components of many shallow-water carbonates throughout Earth’s his...
The shallow carbonate facies at the top of the Yacoraite Formation (Late Cretaceous–Early Palaeocene...
The architecture of lacustrine systems is the result of the complex interaction between tectonics, c...
Due to the complex nature and importance of porosity in carbonate systems, it has been extensively s...
Ooids, pisoids, nodules, concretions, and a host of other terms are used to describe concentrically-...
743-758This study is an attempt to describe the distribution and fabric of the Cambrian ooids from t...
International audienceIn this study, an integrated approach was applied using available sedimentary,...
In this study, an integrated approach was applied using available sedimentary, geochronology, geoche...
Ooids are a common type of carbonate sand grain that form through a combination of constructive and ...
Ocean Anoxic Events (OAEs) are major carbon cycle perturbations that occurred several times in the M...
The Carmel Formation formed in a shallow inland sea during the Middle Jurassic and is located in par...