Results 161 to 170 of about 16,460 (227)

The Deep Subsurface Biosphere and its Substrates Along a One-Million-Year Ferruginous Lake Archive. [PDF]

Microb Ecol
Ruiz-Blas F, Friese A, Bartholomäus A, Henny C, Russell JM, Kallmeyer J, Vuillemin A.   +6 more
europepmc   +1 more source

Tracking lithospheric delamination and surface processes across the Messinian salinity crisis. [PDF]

Nat Commun
Mouthereau F, Boschetti L, Larrey M, Brichau S, Beaudoin NE, Huyghe D, Roberts NMW, Daëron M.   +7 more
europepmc   +1 more source

Earthquake rupture variability along the central seismic gap segment (78°- 82°E) of the Himalayan Frontal Thrust, Western and Central Himalaya. [PDF]

Sci Rep
Arora S, Meenan N, Srivastava E, Cochran D, Singh G, Williams A, Dhali M, Kumaiya M, Arrowsmith R, Malik JN, Kondo H.   +10 more
europepmc   +1 more source

Sedimentation in Meridiani Terrae, Mars, owing to magma-ice interaction when Tharsis arose? [PDF]

, 2004
Grady, M., Nussbaumer, J.
core  

Tectonics and Sedimentation of the Meso- to Neoproterozoic Timan-Varanger Belt along the Northeastern Margin of Baltica [PDF]

, 2000
Olovyanishnikov, V. G., Roberts, D., Siedlecka, A.   +2 more
core  

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]

Environ Sci Pollut Res Int
Novak M, Kochergina YVE, Andronikov AV, Holmden C, Veselovsky F, Kachlik V, Hruška J, Laufek F, Paces T, Komarek A, Sebek O, Stepanova M, Curik J, Prechova E, Fottova D, Andronikova IE.   +15 more
europepmc   +1 more source

Anatomy of the magmatic-hydrothermal system beneath Uturuncu volcano, Bolivia, by joint seismological and petrophysical analysis. [PDF]

Proc Natl Acad Sci U S A
Liu Y, Kendall JM, Zhang H, Blundy JD, Pritchard ME, Hudson T, MacQueen P.   +6 more
europepmc   +1 more source

Biostratigraphy and palaeoenvironments of the Upper Cretaceous fossil fish Konservat-Lagerstätten of Lebanon

Maksoud S, Hossny TE, Samankassou E, Cavin L, Saad PA, Azar D, Piuz A.   +6 more
europepmc   +1 more source

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Eustatic control of turbidites and winnowed turbidites

Geology, 1982
Global 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.
G. Shanmugam, R. J. Moiola
openaire   +1 more source