Results 181 to 190 of about 201,729 (304)
ABSTRACT Features considered indicative of hyperpycnites and intrabasinal turbidites overlap. Outcrop study presented here suggests that the Westward Ho! Formation forms an 800 m high deepwater‐slope system dominated by hyperpycnites. Taking this unit, and other successions where hyperpycnites have been described, as having been deposited solely from ...
Tony Reynolds
wiley +1 more source
Methodological workflow for assessing heterogeneity in immature organic-rich carbonate reservoirs. [PDF]
Aljurf S, Abu-Mahfouz IS, Chan S.
europepmc +1 more source
ABSTRACT The Paleoarchean Antarctic Creek Member of the Mount Ada Basalt, Eastern Pilbara Terrane, Western Australia, includes beds of jasper and white chert composed of sand‐sized silica granules that often contain or are mixed with silt‐sized particles of haematite.
Donald R. Lowe, Gary R. Byerly
wiley +1 more source
Compound Heterozygous Hemoglobin E-Beta (HbE-β)-Thalassemia Presenting With Chipmunk or Rodent Facies, and a Severe Thalassemia Major Phenotype. [PDF]
Dutta A, Banik A, Das D, Dutta TS.
europepmc +1 more source
Grain-size analysis of samples from Cape Roberts core CRP-3, Victoria Land Basin, Antarctica [PDF]
Barrett, P. J.
core
ABSTRACT Understanding the processes that drive soil formation is crucial for developing sustainable land‐use strategies, as changing land‐use practices and climate change exacerbate soil erosion. The formation of substantial arable soils on carbonate bedrock requires substantial dust accretion as the underlying bedrock lacks siliciclastic material. In
Daniel Palchan +3 more
wiley +1 more source
A study on a screening and diagnostic model for adenoid faces based on an improved convolutional neural network. [PDF]
Wang Y, Gao D, He J, He J, Wu J.
europepmc +1 more source
Glacial geomorphology: the paleozoic sedimentary successions of Northern Ethiopia [PDF]
Bheemalingeswara, Konka +2 more
core +1 more source
ABSTRACT The Paleoproterozoic Talvivaara mudstone is a very large sulfidic Ni‐Co deposit that records enhanced organic matter accumulation during the global Shunga Event. Here, rock geochemistry and microscale S and Fe isotope composition of in situ pyrrhotites and pyrites are studied in well‐characterised, well‐preserved drill core samples.
Raimo Lahtinen +3 more
wiley +1 more source

