[HTML][HTML] Tracing volcanic emissions from the Central Atlantic Magmatic Province in the sedimentary record
The end-Triassic mass extinction (ETME) is thought to have been caused by voluminous,
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …
A review of Pangaea dispersal and Large Igneous Provinces–In search of a causative mechanism
The breakup of Pangaea was accompanied by extensive, episodic, magmatic activity.
Several Large Igneous Provinces (LIPs) formed, such as the Central Atlantic Magmatic …
Several Large Igneous Provinces (LIPs) formed, such as the Central Atlantic Magmatic …
Kinematic evolution of the southern North Atlantic: Implications for the formation of hyperextended rift systems
We focus on the southern North Atlantic rifted margins to investigate the partitioning and
propagation of deformation in hyperextended rift systems using plate kinematic modeling …
propagation of deformation in hyperextended rift systems using plate kinematic modeling …
The Triassic–Jurassic transition–A review of environmental change at the dawn of modern life
Abstract The Triassic–Jurassic transition, which is here broadly defined as extending from
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
The Tell-Rif orogenic system (Morocco, Algeria, Tunisia) and the structural heritage of the southern Tethys margin
R Leprêtre, D Frizon de Lamotte… - BSGF-Earth …, 2018 - pubs.geoscienceworld.org
The Tell-Rif (Tell in Algeria and Tunisia; Rif in Morocco) is the orogenic system fringing to
the south the West Mediterranean basins. This system comprises three major tectonic …
the south the West Mediterranean basins. This system comprises three major tectonic …
Mesozoic rifting evolution of SW Gondwana: a poly-phased, subduction-related, extensional history responsible for basin formation along the Argentinean Atlantic …
The opening of the South Atlantic in the Early Cretaceous was the final stage of the complex
rifting history of SW Gondwana. In this contribution we reassess the chronology of Mesozoic …
rifting history of SW Gondwana. In this contribution we reassess the chronology of Mesozoic …
Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary
P Angrand, F Mouthereau - BSGF-Earth Sciences …, 2021 - pubs.geoscienceworld.org
Abstract The West European collisional Alpine belts are the result of the inversion, initiated
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
[HTML][HTML] A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
The western European kinematic evolution results from the opening of the western
Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological …
Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological …
The Ivrea-Verbano tectonic evolution: The role of the crust-mantle interactions in rifting localization
This work aims to review and discuss with new interpretations the tectonic evolution of the
Ivrea Verbano Zone (IVZ), to highlight how inheritance from previous orogenic cycles may …
Ivrea Verbano Zone (IVZ), to highlight how inheritance from previous orogenic cycles may …
Paleostress constraints on the tectonic evolution of the Central High Atlas orogen
Abstract The Central High Atlas is distinguished by map-scale, sigmoid, and narrow
magmatic-cored ridges, which separate wide and open synclines. The origin of these …
magmatic-cored ridges, which separate wide and open synclines. The origin of these …