Late Miocene megalake regressions in Eurasia
The largest megalake in the geological record formed in Eurasia during the late Miocene,
when the epicontinental Paratethys Sea became tectonically-trapped and disconnected from …
when the epicontinental Paratethys Sea became tectonically-trapped and disconnected from …
Human occupation of northern Europe in MIS 13: Happisburgh Site 1 (Norfolk, UK) and its European context
SG Lewis, N Ashton, MH Field, PG Hoare… - Quaternary Science …, 2019 - Elsevier
The timing, environmental setting and archaeological signatures of an early human
presence in northern Europe have been longstanding themes of Palaeolithic research. In …
presence in northern Europe have been longstanding themes of Palaeolithic research. In …
[HTML][HTML] A persistent non-uniformitarian paleomagnetic field in the Devonian?
The Devonian has long been a problematic period for paleomagnetism. Devonian
paleomagnetic data are generally difficult to interpret and have complex partial or full …
paleomagnetic data are generally difficult to interpret and have complex partial or full …
Paleomagnetic rotations in the northeastern Caribbean region reveal major intraplate deformation since the Eocene
Abstract Relative Caribbean‐North American plate motion is partitioned over the trench and
intra‐Caribbean plate faults that bound large scale tectonic blocks. Quantifying the kinematic …
intra‐Caribbean plate faults that bound large scale tectonic blocks. Quantifying the kinematic …
Kinematic and paleomagnetic restoration of the Semail ophiolite (Oman) reveals subduction initiation along an ancient Neotethyan fracture zone
DJJ Van Hinsbergen, M Maffione… - Earth and Planetary …, 2019 - Elsevier
The archetypal Semail ophiolite of Oman has inspired much thought on the dynamics of
initiation of intra-oceanic subduction zones. Current models invoke subduction initiation at a …
initiation of intra-oceanic subduction zones. Current models invoke subduction initiation at a …
Cenozoic rotation history of Borneo and Sundaland, SE Asia revealed by paleomagnetism, seismic tomography, and kinematic reconstruction
SE Asia comprises a heterogeneous assemblage of fragments derived from Cathaysia
(Eurasia) in the north and Gondwana in the south, separated by suture zones representing …
(Eurasia) in the north and Gondwana in the south, separated by suture zones representing …
Integrated bio-magnetostratigraphy of the Badenian reference section Ugljevik in southern Pannonian Basin-implications for the Paratethys history (middle Miocene …
Abstract The Central Paratethys was a large-scale Oligo-Miocene epicontinental sea located
in Central and Eastern Europe. It was separated from the Mediterranean by the Alpine …
in Central and Eastern Europe. It was separated from the Mediterranean by the Alpine …
Paleomagnetic evidence for upper plate response to a STEP fault, SW Anatolia
Abstract Pliny-Strabo Trench is a Subduction Transform-Edge Propagator (STEP) Fault
developed on the northern edge of the subducted African Oceanic Lithosphere. It connects …
developed on the northern edge of the subducted African Oceanic Lithosphere. It connects …
Conceptual models for short‐eccentricity‐scale climate control on peat formation in a lower Palaeocene fluvial system, north‐eastern Montana (USA)
LJ Noorbergen, HA Abels, FJ Hilgen… - …, 2018 - Wiley Online Library
Fluvial systems in which peat formation occurs are typified by autogenic processes such as
river meandering, crevasse splaying and channel avulsion. Nevertheless, autogenic …
river meandering, crevasse splaying and channel avulsion. Nevertheless, autogenic …
[HTML][HTML] From Khersonian drying to Pontian “flooding”: late Miocene stratigraphy and palaeoenvironmental evolution of the Dacian Basin (Eastern Paratethys)
In the late Miocene, a large inland sea known as the Eastern Paratethys stretched out across
the present-day Black Sea–Caspian Sea region. The basin was mostly endorheic and its …
the present-day Black Sea–Caspian Sea region. The basin was mostly endorheic and its …