Results 121 to 130 of about 886 (180)

Microscopic Characteristics and Controlling Factors of Pore Structures in Shale Reservoirs: A Case Study of the Chang 7 Member in the Longdong Area of the Ordos Basin. [PDF]

ACS Omega
Li G, He W, Wen Z, Hu Y, Gao X, Xiao N.
europepmc   +1 more source

Pitfalls and opportunities in estimating the volumes of small, young submarine landslides

Urlaub M, Sager TF, Berndt C.
europepmc   +1 more source

A microscopic Burgess Shale: small carbonaceous fossils from a deeper water biota and the distribution of Cambrian non-mineralized faunas. [PDF]

Proc Biol Sci
Mussini G, Butterfield NJ.
europepmc   +1 more source

A study on the accumulation model of the Santos basin in Brazil utilizing the source-reservoir dynamic evaluation method. [PDF]

Sci Rep
Yan K, Zuo Y, Zhang Y, Yang L, Pang X, Wang S, Li W, Song X, Yao Y.   +8 more
europepmc   +1 more source

High latitude terrestrial carbon isotope and mercury perturbations across the Late Triassic Carnian Pluvial Episode in Northwestern China. [PDF]

Sci Rep
Haserbek T, Tian L, Huang J, Shu W, Liu Y, Hua X, Kemp DB, Roghi G, Alverà G, Gianolla P, Du Y, Song H, Song H, Chu D, Cao Y, Shi Y, Dal Corso J.   +16 more
europepmc   +1 more source

Identifying the topographic signature of early Martian oceans. [PDF]

Nature
Zaki AS, Lamb MP.
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Time-dependent probabilistic tsunami risk assessment: application to Tofino, British Columbia, Canada, subjected to Cascadia subduction earthquakes. [PDF]

NPJ Nat Hazards
Goda K, De Risi R.
europepmc   +1 more source

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Ichnocoenoses of a turbidite sole

Ichnos, 1991
Specimens of 13 ichnospecies and their spatial distributions were analyzed on a spectacular cast of a turbidite sole surface (2.9 m2), from Eocene flysch of Spain. The distribution tends to be patchy. Except for postturbidite Granularia, no intraspecies overcrossing was observed.
Stanisław Leszczynski, Adolf Seilacher   +1 more
exaly   +2 more sources

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