Results 171 to 180 of about 95,502 (229)
ABSTRACT This research examines the spatial and geochemical interactions between mat‐forming microorganisms and thalassinid shrimp in an intertidal flat situated on the shores of Willapa Bay, Washington, USA. The study serves as a contemporary analog for the relationships between mats and burrowing organisms in deep time.
Brette S. Harris +9 more
wiley +1 more source
Stratigraphy and Porosity Modeling of South-Central Illinois (USA) Chester (Upper Mississippian) Series Sandstones Using Petrel [PDF]
Darren Kimple +2 more
openalex +1 more source
ABSTRACT Tubular and curviplanar structures, outlined by the occurrence of haematite/goethite, chlorite, quartz and albite, are developed in the Middle Permian Broughton Formation in the southern Sydney Basin, New South Wales, Australia. These structures are interpreted as fluid‐flow pathways resulting from the ejection of heated pore fluids as a thick
Paul F. Carr +5 more
wiley +1 more source
Experimental observations of vertical segregation of sands in oscillatory flows
ABSTRACT Measurements assessing the composition of bed sands under oscillatory flows were conducted in the large wave flume (Großer Wellenkanal, GWK) in Hannover, focusing on diverse sand mixtures. The experiments featured velocity‐asymmetric flows with a consistent wave period of 7 s, while considering two distinct wave heights (1 and 1.5 m). The sand
Tiago Abreu +4 more
wiley +1 more source
ABSTRACT Mongolia's Eastern and Western Gobi Basins preserve a globally significant record of Cretaceous terrestrial vertebrates, yet their biostratigraphic correlations are complicated by a complex geological history. The Eastern Gobi Basin, a northeast‐southwest trending fault‐bounded rift system, includes several minor sub‐basins with distinct ...
Ryan T. Tucker +9 more
wiley +1 more source
ABSTRACT Preserved allocyclic signatures in the rock record often reflect basin‐scale climatic variability and serve as key proxies for correlating ancient dryland successions. The notion of climate cyclicity, however, remains largely untested on regionally constrained, outcrop‐calibrated studies.
Oliver Button +4 more
wiley +1 more source
ABSTRACT The early Miocene unconformity (EMU) formed during a transition in the tectonic regime of western North America that coincided with faunal diversification. The Railroad Canyon section in the northern Rocky Mountains provides a complete geologic record around this event. Our new magnetostratigraphic study in combination with published U‐Pb ages
Dieke Gerritsen +3 more
wiley +1 more source

