Relevant bibliographies by topics / Palermo Pluton

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  2. Dissertations / Theses

Academic literature on the topic 'Palermo Pluton'

Author: Grafiati
Published: 4 June 2021
Last updated: 8 February 2022

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Journal articles on the topic "Palermo Pluton"

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Lü, Zhao-Ying, Chang-Qian Ma, Yuan-Yuan Liu, et al. "Petrogenesis of the Jurassic Guiping Complex in the Southwestern South China Block: Insights into the Subduction Processes of the Paleo-Pacific Slab." Minerals 11, no. 8 (2021): 807. http://dx.doi.org/10.3390/min11080807.

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Late Jurassic NE-trending A-type granitoids are widespread in the Shihang belt, South China, though their petrogenesis and geodynamic settings remain controversial. The Guiping complex is located on the southwest margin of the Shihang belt. In this study, the petrography, major and trace element geochemistry, whole-rock Sr-Nd isotopes, and zircon U-Pb geochronology of the Guiping complex were investigated. The Guiping complex is composed of the Fenghuangling and Xishan plutons; both plutons yielded zircon U-Pb ages of ca. 160 Ma. The Fenghuangling pluton has low SiO2 content of 54.26% to 60.31
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Tan, Jun, Jun-Hao Wei, Shao-Qing Zhao, et al. "Petrogenesis of Late Triassic high-Mg diorites and associated granitoids with implications for Paleo-Tethys evolution in the northeast Tibetan Plateau." GSA Bulletin 132, no. 5-6 (2019): 955–76. http://dx.doi.org/10.1130/b35225.1.

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Abstract Recent research on Paleo-Tethys tectonics has identified a huge late Paleozoic to Mesozoic igneous belt that extends more than 2500 km in the northeast Tibetan Plateau. However, the magma genesis and evolution in this belt remains a subject of considerable debate. This paper presents a combination of zircon U-Pb ages, mineral compositions, major and trace element concentrations, and Sr-Nd-Hf isotopic data for the plutons across the Zhiduo arc belt that marks the site connecting different tectonic-magmatic units. The studied rocks from one quartz diorite, two granodiorite plutons, and
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Lin, Wei, and Qingchen Wang. "Late Mesozoic extensional tectonics in the North China block: a crustal response to subcontinental mantle removal?" Bulletin de la Société Géologique de France 177, no. 6 (2006): 287–97. http://dx.doi.org/10.2113/gssgfbull.177.6.287.

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Abstract In the North China block, Cretaceous extensional tectonics is expressed by numerous syntectonic plutons bounded by ductile normal faults and several metamorphic core complexes (MCC). Cretaceous half-grabens filled by continental terrigenous deposits are widespread. The examples of MCC from South Liaoning Peninsula, Yiwulüshan, Hohhot as well as the Yunmengshan syntectonic pluton spread along ca 2000 km suggest that the early Cretaceous extensional tectonics in the North China block is globally symmetric. The geodynamics setting of this continental-scale extension remains disputed. It
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EMILIA YOLANDA AGUILERA, AGUSTINA REATO, OSCAR MARTÍNEZ, EUGENIO ARAGÓN, and JORGE RABASSA. "GRANITIC LANDSCAPE IN THE MUNRO PLUTON (TAPERA DE BURGOS), PROVINCE OF CHUBUT, PATAGONIA, ARGENTINA." William Morris Davis – Revista de Geomorfologia 1, no. 1 (2020): 47–74. http://dx.doi.org/10.48025/issn2675-6900.v1n1.p47-74.2020.

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The Munro Pluton is located in the extra-Andean region of the province of Chubut, Argentina, in northern Patagonia, northeast of the Sierra de Tecka and northwest of the Sierra de Languineo. It is a sub-volcanic pluton with a SHRIMP age of 60 Ma (Paleocene?). Studies of fission tracks on apatites of the studied region suggest that the exhumation of the region took place during the Paleogene, indicating that the lapse since its emplacement until its exhumation, took less than 35 Ma, and that the pluton has been exposed to weathering at least since the Miocene until present times. This pluton ha
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Dahlquist, Juan A., Sebastián O. Verdecchia, Edgardo G. Baldo, et al. "Early Cambrian U-Pb zircon age and Hf-isotope data from the Guasayán pluton, Sierras Pampeanas, Argentina: implications for the northwestern boundary of the Pampean arc." Andean Geology 43, no. 1 (2016): 137. http://dx.doi.org/10.5027/andgeov43n1-a08.

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An Early Cambrian pluton, known as the Guasayán pluton, has been identified in the central area of Sierra de Guasayán, northwestern Argentina. A U-Pb zircon Concordia age of 533±4 Ma was obtained by LA-MC-ICP-MS and represents the first report of robustly dated Early Cambrian magmatism for the northwestern Sierras Pampeanas. The pluton was emplaced in low-grade metasedimentary rocks and its magmatic assemblage consists of K-feldspar (phenocrysts)+plagioclase+quartz+biotite, with zircon, apatite, ilmenite, magnetite and monazite as accessory minerals. Geochemically, the granitic rock is a metal
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Paterson, S. R., and R. B. Miller. "Stoped blocks in plutons: paleo-plumb bobs, viscometers, or chronometers?" Journal of Structural Geology 20, no. 9-10 (1998): 1261–72. http://dx.doi.org/10.1016/s0191-8141(98)00066-2.

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Dong, Yang, Jingdang Liu, Yanfei Zhang, et al. "Early Cretaceous Xiuyan adakitic granitoids in the Liaodong Peninsula, eastern China: petrogenesis and implications for lithospheric thinning of the North China Craton." Canadian Journal of Earth Sciences 58, no. 1 (2021): 50–66. http://dx.doi.org/10.1139/cjes-2020-0033.

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Mesozoic magmatic rocks are widely distributed in the North China Craton (NCC) and are crucial to understanding the timing, location, and geodynamic mechanisms of lithospheric thinning of the NCC. In this study, we report geochronological, petrogeochemical, and Lu–Hf isotopic data for adakitic granitoids from different parts of Xiuyan pluton in the Liaodong Peninsula, aiming to constrain their magma sources, petrogenesis, and tectonic implications. The adakites are metaluminous to weakly peraluminous and are classified as high-K calc-alkaline I-type granite with Early Cretaceous zircon U–Pb ag
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Murphy, John M., and Arne Bakke. "Low-temperature thermal history of the Gilmore Dome area, Fairbanks Mining District, Alaska." Canadian Journal of Earth Sciences 30, no. 4 (1993): 764–68. http://dx.doi.org/10.1139/e93-062.

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Eight apatite and two zircon fission-track ages provide evidence of complex Tertiary thermal overprinting by hydrothermal fluids in the Gilmore Dome area. Five ages on apatite from the Fort Knox gold deposit average 41 Ma, one from the Stepovich prospect is 80 Ma, and two from Pedro Dome average 67 Ma. Elevations of these samples overlap but their ages do not, indicating that each area experienced a different thermal history.Ages of apatite from the Fort Knox gold deposit decrease with elevation from 42 to 36 Ma but have data trends indicative of complex cooling. Two ~51 Ma ages on zircon indi
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WANG, YINGDE, FENGYUE SUN, LIANG LI, RUIHUA LI, JIAN WANG, and WEI XIN. "Geochronology, geochemistry, and geological implications of late Carboniferous – early Permian mafic and felsic intrusive rocks from Urad Zhongqi, western Inner Mongolia." Geological Magazine 152, no. 6 (2015): 1057–72. http://dx.doi.org/10.1017/s0016756815000138.

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AbstractThe mafic and felsic Haertaolegai intrusions crop out in Urad Zhongqi, western Inner Mongolia and are dominated by monzogranite, porphyritic granite, and gabbroic diorite intrusions. We investigate the tectonic setting, geochronology, and anorogenic characteristics of the western Inner Mongolia through field investigation, microscopic and geochemical analyses of samples from the Haertaolegai bimodal intrusions and laser ablation multi-collector inductively coupled plasma mass spectrometry (LA-MC-ICP-MS) zircon U–Pb dating of gabbroic diorite and adakitic granites. Petrographic and geoc
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Tao, Lu, Fa-Bin Pan, Rong Liu, Chong Jin, Bao-Jian Jia, and Xiaobo He. "Petrogenesis of the Cretaceous granitoids in Zhejiang, northeast South China Block and their implications for episodic retreat and roll-back of the Paleo-Pacific Plate." GSA Bulletin 132, no. 7-8 (2019): 1514–36. http://dx.doi.org/10.1130/b35426.1.

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Abstract Two Cretaceous granitoid belts (i.e., the northwest and southeast belts) have been identified in Zhejiang, northeast South China Block. In this study, seven granitoid plutons from both the two belts were collected for zircon U-Pb dating, whole-rock geochemistry, Sr-Nd isotope, and zircon Hf isotope analyses. Chronologically, the Longyou (132 Ma), Sucun (136 Ma), Shanghekou (131 Ma), and Huangshitan (ca. 126 Ma) plutons from the northwest belt display older magma crystallization age than those of the Xiaoxiong (100 Ma), Zhujiajian (108 Ma), and Qingbang island (108 Ma) plutons from the
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Dissertations / Theses on the topic "Palermo Pluton"

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Crisma, Pedro Rabello. "Petrologia e Mineralogia de rochas graníticas e gabrodioríticas dos plutons Palermo e Rio Negro, região do Alto Rio Negro, PR-SC, Província Graciosa." Universidade de São Paulo, 2013. http://www.teses.usp.br/teses/disponiveis/44/44143/tde-06122013-155433/.

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Os Plutons Palermo (ca. 250 km2) e Rio Negro (ca. 130 km2) afloram na região Alto Rio Negro (PR) e fazem parte da Província Graciosa, uma província Neoproterozóica (ca. 580 Ma) constituída por granitos e sienitos na região S-SE do Brasil. Em ambos os plutons afloram variedades de rochas graníticas, predominantes, e gabro-dioríticas, bem como rochas híbridas, principalmente granodioritos. Estes plutons apresentam zonamento em geral bem marcado, que é tipicamente inverso caso do Pluton Rio Negro. As rochas graníticas principais correspondem a sieno- e monzogranitos predominantes e
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