Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Maria Paula Iglesia Llanos"'
Publikováno v:
Newsletters on Stratigraphy. 56:157-185
Autor:
Federico González Tomassini, Maria Paula Iglesia Llanos, Ivan Lanusse Noguera, Dolores Vallejo, Diego Alejandro Kietzmann, Hernán M. Reijenstein
Publikováno v:
Cretaceous Research. 127:104950
This work presents the first regional biostratigraphic study on the calpionellid zones and assemblages of the Tithonian–lower Valanginian interval in the Neuquen Basin, Southern Andes, Western Argentina. The lower Tithonian–lower Valanginian in t
Autor:
Diego Alejandro Kietzmann, Juan Pablo Palacio, Magalí Aldana Sturlesi, Maria Paula Iglesia Llanos
Publikováno v:
Journal of South American Earth Sciences. 109:103267
This paper presents a multidisciplinary study of a new basinal section of Tithonian-Berriasian the Vaca Muerta Formation at Las Tapaderas area, including detailed, biostratigraphic, sedimentologic, sequence stratigraphic and cyclostratigraphic analys
Publikováno v:
Journal of South American Earth Sciences. 100:102622
We present the oldest record of crustacean microcoprolites in the Neuquen Basin, and the first record of these coprolites for the Bajocian–Callovian of South America. They correspond to three crustacean microcoprolite ichnospecies in prodelta and t
Fil: Kietzmann, Diego Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Bu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4a8d0e7a2e55a05900b481da8b5c4aae
https://www.sciencedirect.com/science/article/pii/S0895981117303449
https://www.sciencedirect.com/science/article/pii/S0895981117303449
Publikováno v:
Stratigraphy & Timescales ISBN: 9780128150986
Detailed cyclostratigraphical analyses have been made from five Tithonian–Berriasian sections of the Vaca Muerta Formation, exposed in the Neuquen Basin, Argentina. The Vaca Muerta Formation is characterized by decimetre-scale rhythmic alternations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad0a7b347f99445c3953d6da7f0db15f
https://doi.org/10.1016/bs.sats.2018.07.003
https://doi.org/10.1016/bs.sats.2018.07.003
Autor:
Andrés Folguera, Eduardo Contreras-Reyes, Nemesio Heredia, Alfonso Encinas, Sofía B. Iannelli, Verónica Oliveros, Federico M. Dávila, Gilda Collo, Laura Giambiagi, Andrei Maksymowicz, María Paula Iglesia Llanos, Martín Turienzo, Maximiliano Naipauer, Darío Orts, Vanesa D. Litvak, Orlando Alvarez, César Arriagada
This book describes the Mesozoic to Cenozoic evolution of the Chilean and Argentinean Andes. The book is structured from a historical perspective concentrating on specific processes explained in each chapter. The chapters cover dynamic subsidence; ne
Publikováno v:
Physics of the Earth and Planetary Interiors. 237:51-64
The most remarkable feature of the Central Andes is the Altiplano–Puna plateau. This plateau is characterized by 3.5 km average elevation, approximately 70 km crustal thickness and very high heat flow. The upper mantle structure changes along strik
Publikováno v:
International Journal of Earth Sciences. 102:745-759
From the Late Carboniferous until the Middle Jurassic, continents were assembled in a quasi-rigid supercontinent called Pangea. The first palaeomagnetic data of South America indicated that the continent remained stationary in similar present-day lat
Autor:
Maria Paula Iglesia Llanos
Publikováno v:
Encyclopedia of Marine Geosciences ISBN: 9789400766440
Magnetic polarity scales younger than 160 Ma are derived from seafloor magnetic anomalies. For older times, such scales must be derived from polarity successions obtained in the continents yielding a precise age control such as that provided by ammon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc5e2c71139a1a012862cf90c0ae35a7
https://doi.org/10.1007/978-94-007-6644-0_71-1
https://doi.org/10.1007/978-94-007-6644-0_71-1