The Deep Subsurface Biosphere and its Substrates Along a One-Million-Year Ferruginous Lake Archive. [PDF]
Ruiz-Blas F +6 more
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Tracking lithospheric delamination and surface processes across the Messinian salinity crisis. [PDF]
Mouthereau F +7 more
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Earthquake rupture variability along the central seismic gap segment (78°- 82°E) of the Himalayan Frontal Thrust, Western and Central Himalaya. [PDF]
Arora S +10 more
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Crustal features of the Claritas Rise region indicate a mobile lithosphere on early Mars
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Anatomy of the magmatic-hydrothermal system beneath Uturuncu volcano, Bolivia, by joint seismological and petrophysical analysis. [PDF]
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Sizeable net export of base cations from a Carpathian flysch catchment indicates their geogenic origin while the 26Mg/24Mg, 44Ca/40Ca and 87Sr/86Sr isotope ratios in runoff are indistinguishable from atmospheric input. [PDF]
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Pitfalls and opportunities in estimating the volumes of small, young submarine landslides
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Eustatic control of turbidites and winnowed turbidites
Geology, 1982Global changes in sea level, primarily the results of tectonism and glaciation, control deep-sea sedimentation. During periods of low sea level the frequency of turbidity currents is greatly increased. Episodes of low sea level also cause vigorous contour currents, which winnow away the fines of turbidites.
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Abstract Deep-water sedimentation is currently a major focus of both academic research and industrial interest. Recent studies have emphasized the fundamental influence of seafloor topography on the growth and morphology of submarine ‘fans’: in many turbidite systems and turbidite hydrocarbon reservoirs, depositional system development has ...
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