Results 81 to 90 of about 207,177 (197)

Long‐Term Increases in Ca2+, Mg2+, and SO42− Concentrations in the Kolyma River (1980–2022) Due To Yedoma Degradation

open access: yesGlobal Biogeochemical Cycles, Volume 40, Issue 2, February 2026.
Abstract Permafrost degradation under a warming climate has altered hydrological and biogeochemical processes across the Arctic. Although increasing fluxes of weathering‐derived ions (e.g., Ca2+, Mg2+, and SO42−) have been reported in Arctic rivers, the underlying mechanisms and hotspots within basins remain poorly understood due to limited analysis of
Y. Tashiro   +10 more
wiley   +1 more source

Oral History Interview with William Belt, December 5, 2005

open access: yes, 2005
The National Museum of the Pacific War presents an oral interview with William Belt. Belt joined the Navy after earning a master's degree and went to midshipman' school. He earned a commission and reported aboard USS Tuscaloosa (CA-37)in May 1943.
Belt, William T.
core  

Where is There Chance to Find Deep Prospects Below the Outer Western Carpathian Thrust Belt?

open access: yes, 2020
In the period of 80 and 90th, the intensive deep drilling and seismic profiling program in the Outer Western Carpathian belt has been realized for confirming the idea about the existence and opening of new promising plays beneath some of these thin ...
Bartoněk, Dalibor   +2 more
core   +1 more source

Kinematic evolution of the Pieniny Klippen Belt in Cenozoic (Ukrainian Carpathians)

open access: yesГеофизический журнал, 2016
The data on surface, subsurface and deep structure of the Pieniny Klippen Belt (PKB) have been summarized and new results of its geological-structural and fault kinematic studies within the Ukrainian part of the Eastern Carpathians have been presented ...
A. V. Murovskaya   +5 more
doaj   +1 more source

Tectono-sedimentary evolution of upper Assam “inter-orogenic” peripheral foreland basin, India

open access: yesDiscover Geoscience
The northern periphery of the Indian craton is the leading edge of the under-thrusting continent in the continent–continent collision set up between the Indian and Eurasian plates.
S. K. Biswas, Gaurav Chauhan
doaj   +1 more source

Heavy mineral analysis of the Upper Cretaceous to Lower Eocene synorogenic formations of the Pieniny Klippen Belt (Šariš Unit, eastern Slovakia): new data from the Jar-2 borehole (Jarmuta-Proč Fm.) and outcrops (Malinowa Fm.)

open access: yesMineralia Slovaca
The study presents new results of heavy mineral analyses including detrital garnet, tourmaline and Cr-rich spinel chemical compositions from the synorogenic Maastrichtian-Ypresian Jarmuta-Proč Fm. of the Šariš Unit of the Pieniny Klippen Belt, penetrated
Jozef Madzin, Dušan Plašienka
doaj   +1 more source

The Neogene evolution of the outer Carpathian flysch units (Poland, Ukraine and Romania): kinematics of a foreland/fold-and-thrust belt system

open access: yesSedimentary Geology, 1993
Abstract Various techniques of geometric and kinematic analyses, including cross-section balancing and forward modeling, have been applied successfully to the outer Carpathian flysch units along regional geologic profiles crossing the belt from its undeformed foreland to the Pieniny klippen belt (western Carpathians, Poland) or to the central east ...
F. Roure, E. Roca, W. Sassi
openaire   +2 more sources

Geology of Tunceli-Bingöl Region of Eastern Turkey

open access: yesBulletin of the Mineral Research and Exploration, 1965
This region is located in the Taurus orogenic belt of the highland district of Eastern Turkey. Lower Permian metasediments and Upper Permian suberystalline limestone are the oldest exposed formations of this region.
F. A. AFSHAR
doaj  

Shallow Seismic Refraction Tomography Images from the Pieniny Klippen Belt (Southern Poland)

open access: yes
The Pieniny Klippen Belt (PKB) is located between the Central and the Outer (Flysch) Carpathians and forms a narrow zone with a complex structure, often described as a mélange.
Jerzy Dec   +3 more
core   +1 more source

Coastal Dinaric Flysch Belt: Paleotransport model for the Pazin Basin and the role of a foreland uplift.

open access: yesNatura Croatica, 1996
Sedimentary infill of the Pazin Basin, Istria, shows that the Eocene foreland basin in coastal Dinarides received the detritus from the outer (Adriatic) side, and not only from the SW indicates the existence of a carbonate area, which was partly exposed and partly covered by shallow sea characterized by carbonate deposition. This high area embraced the
Babić, Ljubomir, Zupanič, Jožica
openaire   +1 more source

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