Results 71 to 80 of about 9,387 (221)

Model of mantle-crust interaction and magma generation in the suprasubduction orogen (Paleozoic of the Urals)

Литосфера, 2018
A model of magma formation in the crust of the Urals mobile belt, which is the best example of epioceanic suprasubduction orogen, has been developed. Magma formation occurs both in the relic oceanic and in the newly formed orogen crust. In the first case
German B. Fershtater, Nadezhda S. Borodina, Fernando Bea, Pilar Montero   +3 more
doaj   +1 more source

Altérabilité expérimentale d'une granodiorite et de son arène en conditions périglaciaire, tempérée et chaude (Experimental alterability of a granodiorite and of its arena under periglacial, temperate and hot conditions)

, 1988
. - A granodiorite and its arena have been experimentally altered by reproducing the thermohydric conditions of periglacial, temperate and hot climates.
Vérague, Jean
core   +1 more source

Camp Creek Revisited, One More Time: Evaluating Multiple Approaches to Quantify Peak Flow Response to Forestry for a Medium‐Size Snow‐Dominated Catchment

Water Resources Research, Volume 62, Issue 9, September 2026.
Abstract Forest disturbance effects on peak flows have been debated for decades. Paired‐catchment analysis (PCA) has been criticized in relation to the long‐term stability of pre‐harvest regressions and the inability of chronological pairing to characterize changes in event frequency.
R. Dan Moore, Kim Green, Cydne Potter
wiley   +1 more source

Simulated organic acid weathering of granodiorite and basalt

, 1989
Basalt and granodiorite (medium to fine sand particle size) were leached by three low molecular weight aliphatic organic acids, namely citric, oxalic and acetic acid of . 1M concentration.
Aceman, Sheila
core   +1 more source

Contact structures at a granodiorite intrusion, Piccaninny Point, north-east Tasmania [PDF]

, 1973
At Piccaninny Point, structures developed at the contact between the Piccaninny Creek Pluton and the Mathinna Beds have, a bearing on the mode of emplacement of this body and other granodiorite plutons in north-eastern Tasmania.
RD Gee (17323540), Groves, DI, DI Groves (15964820), Gee, RD   +3 more
core   +1 more source

Geochemical Characteristics of the Granodiorite Porphyry in Dongxiang W-Cu Deposit, SE China

, 2023
The Dongxiang tungsten–copper deposit is a large W–Cu deposit located in the northeast of Jiangxi province in south China. Previous studies have mainly considered the geochemical and isotopic attributes of the ore deposit, but information is ...
Pei Ni, Yitao Cai, Guoguang Wang, Hui Chen   +3 more
core   +1 more source

Resolving Micrometre‐Scale Zircon Growth in Silicic Systems by 7 μm LA‐MC‐ICP‐MS U‐Pb Dating: Linking Petrology and Geochronology in Silicic Volcanic and Granitic Rocks from Victoria, Australia

Geostandards and Geoanalytical Research, Volume 50, Issue 3, Page 625-647, September 2026.
Key Points 7 μm spot‐diameter LA‐MC‐ICP‐MS analyses yield accurate zircon U‐Pb ages. 1013 Ω amplifier resistors improve low‐signal Pb measurements. Saturn correction protocols minimise down‐hole fractionation effects. We present a systematic evaluation of high spatial‐resolution zircon U‐Pb dating using a Thermo Scientific Neoma multi‐collector ICP‐MS ...
Cristiano Lana, John D. Clemens
wiley   +1 more source

Petrogenesis and Metallogenic Implications of Neoproterozoic Granodiorite in the Super-Large Shimensi Tungsten-Copper Deposit in Northern Jiangxi, South China

, 2018
The newly discovered Shimensi deposit is a super-large tungsten-copper (W–Cu) deposit with a metal reserve of 742.55 thousand tonnes (kt) W and 403.6 kt Cu.
Lei Liu, Wenfeng Wei, Xiaoxi Zhu, Zhu, Xiaoxi, Bing Yan, Lai, Chunkit, Yan, Bing, Chunkit Lai, Wei, Wenfeng, Song, Shengqiong, Liu, Lei, Shengqiong Song   +11 more
core   +1 more source

Nd-Sr Isotopic Geochemistry and U-Pb Geochronology of the Fé Granitic Gneiss and Lajedo Granodiorite: Implications for Paleoproterozoic Evolution of the Mineiro Belt, Southern São Francisco Craton, Brazil [PDF]

Geologia USP. Série Científica, 2008
The Fé granitic gneiss and Lajedo granodiorite belong to a voluminous felsic-mafic plutonism, tectonically linked toPaleoproterozoic magmatic evolution of the Mineiro Belt, southern portion of the São Francisco Craton, central-easternBrazil.
Wilson Teixeira, Ciro Alexandre Ávila, Luciana Cabral Nunes   +2 more
doaj  

Petrology, geochemistry and tectonic setting studies in magmatic complex generating the Takht Fe-skarn deposit, NE Hamedan

Journal of Economic Geology, 2019
Introduction The Urumieh-Dokhtar Magmatic Assemblage (UDMA) forms a distinct NW-SE linear intrusive–extrusive complex Magmatism of the UDMA that occurred from Eocene to Quaternary, although the maximum activity was in the middle Eocene (Berberian and ...
Seyed Nematollah Haghighi Bardineh, Reza Zarei Sahamieh, Hassan Zamanian, Ahmad Ahmadi Khalaji   +3 more
doaj   +1 more source