نتایج جستجو برای: magnetostratigraphy

تعداد نتایج: 280  

Journal: :Palaeogeography, Palaeoclimatology, Palaeoecology 2021

Abstract The principal objective of the Hominin Sites and Paleolakes Drilling project (HSPDP) is to study relationship between climate environmental change implications on human evolution in eastern Africa. For this purpose, HSPDP has recovered a 228 m core Chemeron Formation Baringo Basin (Kenya). spans approximately 3.7 Myr, from around 1.6 5.3 Ma, yielded many vertebrate fossils, including f...

1997
D. W. Burbank

M. Mange Department of Earth Sciences, University of Oxford, Parks Road, Oxford, OX1 3PR, England Abstract This integrated study of the sedimentology, magnetostratigraphic chronology and petrography of the mostly continental clastics of the Oligocene to Miocene Swiss Molasse Basin underpins a reconstruction of facies architecture and delineates relationships between the depositional evolution o...

2012
Tao Li Jie Chen Jessica A. Thompson Douglas W. Burbank Weipeng Xiao

[1] Across contractional orogens, the equivalency between decadal convergence rates from geodetic GPS data and geologic shortening rates at time scales of thousands or millions of years has rarely been documented. Here, we present an example from the northern margin of Chinese Pamir, where the Main Pamir Thrust is tectonically quiescent, and recent deformation is concentrated on the Pamir Front...

2013
SPENCER G. LUCAS

The current Triassic chronostratigraphic scale is a hierarchy of three series divided into seven stages, divided further into 15 substages. Ammonoid and conodont biostratigraphies provide the primary basis for chronostratigraphic definition based on global stratotype sections and points (GSSP). I propose that Triassic chronostratigraphic definition should rely entirely on ammonoid biochronologi...

2012
E. M. Roberts N. J. Stevens P. M. O’Connor P. H. G. M. Dirks M. D. Gottfried W. C. Clyde R. A. Armstrong A. I. S. Kemp

The East African Rift System transects the anomalously high-elevation Ethiopian and East African plateaux that together form part of the 6,000-km-long African superswell structure. Rifting putatively developed as a result of mantle plume activity that initiated under eastern Africa. The mantle activity has caused topographic uplift that has been connected to African Cenozoic climate change and ...

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