Results 121 to 130 of about 776 (184)

Orogenic structure and topography track subduction singularities during slab delemination and detachment. [PDF]

Sci Rep
Handy MR.
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Middle Pleistocene tectonic events around the SE Aegean Sea: Insights from magnetostratigraphy, (U-Th)/He zircon dating, and fault kinematics in the Datça Graben (SW Türkiye). [PDF]

Sci Rep
İnce MD, Kaymakci N, Langereis C, Uzel B, Gülyüz E, Koralay EO, Stoica M, Sümer Ö.   +7 more
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Grain orientation in turbidites

The Journal of the Geological Society of Japan, 1969
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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
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Discovery of White Sea assemblage fossils from Laurentia. [PDF]

Sci Adv
Evans SD, Sperling EA, Lau KV, Strauss JV.   +3 more
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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
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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]

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
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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
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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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Scaling in turbidite deposition

Journal of Sedimentary Research, 1994
Abstract We propose that the distribution of layer thicknesses of turbidite deposits that show minimal erosional truncation and amalgamation should obey the power law N(h) congruent to h (super -B) , where N(h) is the number of layers of thickness greater than h and B congruent to 1.
Daniel H. Rothman, John P. Grotzinger, Peter Flemings   +2 more
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