Results 161 to 170 of about 16,283 (208)

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

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

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  

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
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Confined turbidite systems

Geological Society, London, Special Publications, 2004
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 ...
Simon A. Lomas, Philippe Joseph
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Vacillatory turbidites, Barbados

Sedimentary Geology, 1988
Abstract A vacillatory turbidite is one containing Bouma sequence divisions that repeat within a bed; it presumably results from a single flow event or several closely-related events (for example, retrogressive slope failure). The most common vacillations or repetitions in such turbidites on Barbados are between T b and T c intervals (T bcbc , for ...
D.K. Larue, K.G. Provine
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Eolian-Sand Turbidites

SEPM Journal of Sedimentary Research, 1977
ABSTRACT Eolian-sand turbidites form a clearly distinguishable "eolomarine" sediment facies. They are almost devoid of gradation, fine fraction, and mica, and have comparatively coarse sand medians. The sands consist predominantly of quartz grains, a significant portion of which show yellowish-red stains and frosted surfaces, both characteristic of ...
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Ten turbidite myths

Earth-Science Reviews, 2002
Abstract During the past 50 years, the turbidite paradigm has promoted many myths related to deep-water turbidite deposition. John E. Sanders (1926–1999), a pioneering process sedimentologist, first uncovered many of these turbidite myths. This paper provides a reality check by undoing 10 of these turbidite myths. Myth No.
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