Results 111 to 120 of about 8,100 (227)
The Indochina-Simao and Yangtze blocks were separated by a branch of the Paleo-Tethys Ocean, commonly referred as the Ailaoshan Ocean in the Paleozoic Remnants of this Ailaoshan Ocean have been variably suggested to locate along (from east to west) the ...
Meffre, Sebastien +5 more
core +1 more source
Abstract Quartz grain surface microtextures serve as robust records of sedimentary history and depositional environment, yet a coherent framework quantitatively linking specific microtextures to stream power remains underexplored. This study integrates scanning electron microscopy (SEM) with quantitative hydrodynamic analysis along the Kinu River ...
W. Dong, H. Itamiya, T. Sugai
wiley +1 more source
Maximum depositional age biased on U-Pb detrital zircon geochronology.
Maximum depositional age biased on U-Pb detrital zircon geochronology.
Jorge Fernando Genise (8375487) +2 more
core +1 more source
The Geologic History of the Chehalis Forearc Basin, Washington State, USA
Abstract The Chehalis basin is located between the Cascade arc and the Coast Range in southwest Washington State. It consists of sedimentary and volcanic rocks deposited throughout the Cenozoic and is underlain by the Siletzia terrane, a thick, large igneous province accreted in the Eocene.
R. L. Moe +3 more
wiley +1 more source
the detrital zircon U-Pb data of the Xiashu loess
Raw data set for all the detrital zircon U-Pb data of the Xiashu loess reported in this ...
chao wu (8670855)
core +1 more source
Provenance of Late Paleozoic-Mesozoic Sandstones, Taimyr Peninsula, the Arctic
The sedimentary and provenance characteristics of seven Permo-Carboniferous and two early Cretaceous samples from the Taimyr Peninsula provide information about the latest evolution of Uralian orogeny and the opening of the Amerasian Basin.
Robert Scott +3 more
doaj +1 more source
Large-number detrital zircon U-Pb ages reveal global cooling caused the formation of the Chinese Loess Plateau during Late Miocene. [PDF]
Zhang H +10 more
europepmc +1 more source
Variable Sr Diffusion and Implications for Rb–Sr Biotite Geochronology
ABSTRACT The rubidium–strontium (Rb–Sr) system has a long pedigree as a geochronological tool that relies on the application of an isochron approach. In particular, biotite contains strongly radiogenic Rb–Sr isotopes, and thus can yield meaningful crystallisation or cooling ages via this approach. However, the response of the Rb–Sr system in biotite to
Riley Rohrer +4 more
wiley +1 more source
The latest Eocene and Oligocene was a time of marked paleoenvironmental change in Taranaki Basin, involving a transition from the accumulation of coal measures and inner shelf deposits to the development of upper bathyal environments. Up until the end of
Hopcroft, Bradley Scott
core
Detrital zircon age of loess from Chinese Loess Plateau
Detrital zircon age of loess from Chinese Loess ...
Hanzhi Zhang (2589490)
core +1 more source

