Search Results - Monzón*

Zircon U-Pb age and Hf isotopic compositions of quartz monzonite and enclosed mafic enclaves in Muchen pluton, Zhejiang Province: tracing magma mixing in their petrogenesis by Liu, L., Qiu, J., Li, Zhen

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Origin of mafic microgranular enclaves (MMEs) and their host quartz monzonites from the Muchen pluton in Zhejiang Province, Southeast China: implications for magma mixing and crust–mantle interaction by Liu, L., Qiu, J., Li, Zhen

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Petrogenesis of the Early Cretaceous quartz monzonite pluton at Muchen in Longyou County, Zhejiang Province: Evidences from elemental and isotopic geochemistry of mafic microgranular enclaves and their host rocks by Liang, L., Jiansheng, Q., Li, Zhen, YouLian, L.

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Late Triassic melting of a thickened crust in southeastern China: Evidence for flat-slab subduction of the Paleo-Pacific plate by Zhu, Kong-Yang, Li, Zheng-Xiang, Xu, X., Wilde, Simon

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Petrogenesis dan geokimia batuan igneus jalur tengah semenanjung Malaysia / Mohd Rozi Umor by Umor, Mohd Rozi

“…Batuan siri alkali terdiri daripada gabro-gabro alkali, piroksenit, diorit-diorit kuarza, sienit-sienit kuarza dan monzonit kuarza. Ia dikelaskan sebagai batuan metalumina, granit jenis-I, shoshonit dan mengandungi kandungan LILE yang tinggi, terutamanya Ba dan Sr. …”
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Complexity of the early Archean Uivak Gneiss: Insights from Tigigakyuk Inlet, Saglek Block, Labrador, Canada and possible correlations with south West Greenland by Salacinska, A., Kusiak, M., Whitehouse, M., Dunkley, Daniel, Wilde, Simon, Kielman, R.

“…Magmatism between these tectono-metamorphic events is recorded by the presence of meta-mafic dykes in the gneisses, gabbroic enclaves in ca. 2.7 Ga syn-tectonic granitoids, as well as by a ca. 3.56 Ga age for monzonitic gneiss in which metamorphic zircon is present as xenocrysts. …”
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Regolith breccia Northwest Africa 7533: Mineralogy and petrology with implications for early Mars by Hewins, R., Zanda, B., Humayun, M., Nemchin, Alexander, Lorand, J., Pont, S., Deldicque, D., Bellucci, J., Beck, P., Leroux, H., Marinova, M., Remusat, L., Göpel, C., Lewin, E., Grange, Marion, Kennedy, Allen, Whitehouse, M.

“…The zircon from the monzonitic rocks has a higher Δ17O than other Martian meteorites explained in part by assimilation of regolith materials enriched during surface alteration (Nemchin et al.). …”
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The world-class Wallaby gold deposit, Laverton, Western Australia: An orogenic-style overprint on a magmatic-hydrothermal magnetite-calcite alteration pipe? by Salier, B., Groves, D., McNaughton, Neal, Fletcher, Ian

“…The conglomerate is intruded by an apparently comagmatic alkaline dyke suite displaying increasing fractionation through mafic-monzonite, monzonite, syenite, syenite porphyry to late-stage carbonatite. …”
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Origin of postcollisional magmas and formation of porphyry Cu deposits in southern Tibet by Wang, R., Weinberg, R., Collins, Bill, Richards, J., Zhu, D.

“…A distinct change in magmatism along the length of the belt occurs at around 88°E in the Miocene suites: to the east, porphyry copper mineralization is associated with a moderately oxidized, high-Sr/Y granitoid suite (suite II, ΔFMQ = +0.8 to +2.9) with minor occurrences of transitional (hybrid) monzonitic (suite III) and trachytic rocks (suite IV; both with zircon Ce4+/Ce3+ > 50–100, EuN/EuN* = ~0.5, and ΔFMQ = ~+1 to +2). …”
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Petrogenesis and tectonic significance of the ~850 Ma Gangbian alkaline complex in South China: Evidence from in situ zircon U-Pb dating, Hf-O isotopes and whole-rock geochemistry by Li, X., Li, W., Li, Q., Wang, Xuan-ce, Liu, Y., Yang, Y.

“…Subsequent fractional crystallization of hornblende and minor amounts of plagioclase from the alkali basaltic magmas, accompanied by crustal contamination, produced the Si-saturated to -oversaturated syenites and quartz monzonites. These ca. 0.85 Ga alkaline rocks and neighboring contemporaneous dolerite dykes are the products of the anorogenic magmatism after the Sibao Orogeny. …”
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Role of mantle-derived magma in genesis of early Yanshanian granites in the Nanling Range, South China: in situ zircon Hf-O isotopic constraints by Li, X., Li, W., Wang, Xuan-ce, Li, Q., Liu, Y., Tang, G.

“…The Lisong MMEs were crystallized from a mantle-derived magma, similar to the parental magma of the Qinghu monzonite, with small amount of crustal assimilation. …”
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Intracontinental Eocene-Oligocene Porphyry Cu Mineral Systems of Yunnan, Western Yangtze Craton, China: Compositional Characteristics, Sources, and Implications for Continental C... by Lu, Y., Kerrich, R., Kemp, A., McCuaig, T., Hou, Z., Hart, C., Li, Zheng-Xiang, Cawood, P., Bagas, L., Yang, Z., Cliff, J., Belousova, E., Jourdan, Fred, Evans, Noreen

“…The Yao’an porphyry Au system, Machangqing porphyry Cu-Mo system, and Beiya porphyry-skarn Au system, are spatially and temporally associated with potassic felsic intrusions emplaced during the Eocene to Oligocene epochs at 37 to 33 Ma in a postcollisional intracontinental setting in western Yunnan, western Yangtze craton, China. The Yao’an monzonite and quartz monzonite porphyry intrusions are alkaline and potassic with high K2O/Na2O ratios (1.1–1.5). …”
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Synchronous crustal growth and reworking recorded in late Paleoproterozoic granitoids in the northern Tarim craton: In situ zircon U-Pb-Hf-O isotopic and geochemical constraints an... by Ge, R., Zhu, W., Wilde, Simon, He, J., Cui, X.

“…Here, we report sensitive high-reso lution ion microprobe (SHRIMP) and laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) zircon U-Pb ages, in situ zircon Hf-O isotopic data, and whole-rock geochemical data for a variety of granitoids, including monzogranite, quartz diorite/quartz monzonite, garnet-bearing granodiorite, tonalite, and trondhjemite. …”
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Late Carboniferous high εNd(t)– εHf(t) granitoids, enclaves and dikes in western Junggar, NW China: Ridge-subduction-related magmatism and crustal growth by Tang, G., Wang, Q., Wyman, D., Li, Zheng-Xiang, Zhao, Z., Yang, Y.

“…We report results of petrologic, geochronological and geochemical investigation of the Late Carboniferous diorites, granodiorites, amphibole (Am)-bearing granites, and associated dioritic and monzonitic enclaves and mafic and granitic dikes in the Keramay area, of the western Junggar region of Central Asian Orogenic Belt (CAOB). …”
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Late Cretaceous (ca. 90 Ma) adakitic intrusive rocks in the Kelu area, Gangdese Belt (southern Tibet): Slab melting and implications for Cu–Au mineralization by Jiang, Z., Wang, Q., Li, Zheng-Xiang, Wyman, D., Tang, G., Jia, X., Yang, Y.

“…These rocks consist of quartz monzonites and diorites. The quartz monzonites, with SiO2 of 58–59 wt.% and Na2O/K2O of 1.1–1.2, are geochemically similar to slab-derived adakites characterized by apparent depletions in heavy rare earth elements (e.g., Yb = 1.4–1.5 ppm) and Y (16–18 ppm) contents, positive Sr but negative Nb and Ti anomalies on multi element variation diagrams. …”
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Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust by Hewins, R., Zanda, B., Humayun, M., Lorand, J., Deldicque, D., Pont, S., Fieni, C., Nemchin, Alexander, Grange, M., Kennedy, A., Goepel, C., Lewin, E.

“…Lithic clasts are pyroxenite, norite and zircon-bearing monzonite. The impact melt can be modeled as a mixture of crystal clasts and is poor in monzonite.…”
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A geochemical study of syn-subduction and post-collisional granitoids at Muzhaerte River in the Southwest Tianshan UHP belt, NW China by Gou, Long-Long, Zhang, L., Tao, R., Du, J.

“…The porphyritic granitoids consist of granite, granodiorite and quartz monzonite, with relatively high SiO 2 (65.94-75.27wt.%) and K 2O+Na 2O (7.55-9.13wt.%), low MgO (0.18-1.22wt.%), and A/CNK ratios of 0.82-1.11. …”
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Geochemical, Sr-Nd-Pb, and Zircon Hf-O Isotopic Compositions of Eocene-Oligocene Shoshonitic and Potassic Adakite-like Felsic Intrusions in Western Yunnan, SW China: Petrogenesis a... by Lu, Yong-Jun, Kerrich, Robert, McCuaig, T. Campbell, Li, Zheng-Xiang, Hart, Craig J.R., Cawood, Peter A., Hou, Zeng-Qian, Bagas, Leon, Cliff, John, Belousova, Elena A., Tang, Suo-Han

“…The shoshonitic syenite and quartz monzonites have the same Sr–Nd–Pb isotope compositions as the shoshonitic mafic volcanic rocks. …”
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Transition from oceanic to continental lithosphere subduction in southern Tibet: Evidence from the Late Cretaceous–Early Oligocene (~91–30 Ma) intrusive rocks in the Chanang–Zedong... by Jiang, Z., Wang, Qiang, Wyman, D., Li, Zheng-Xiang, Yang, J., Shi, X., Ma, L., Tang, G., Gou, G., Jia, X., Guo, H.

“…The younger (~ 30 Ma) Chongmuda adakitic quartz monzonites and minor granodiorites were most probably derived by partial melting of Early Oligocene northward-subducted Indian lower crust beneath the southern Lhasa Block. …”
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Revisiting the “C-type adakites” of the Lower Yangtze River Belt, central eastern China: In-situ zircon Hf–O isotope and geochemical constraints by Li, X., Li, Zheng-Xiang, Li, W., Wang, Xuan-Ce, Gao, Y.

“…These “C-type adakitic rocks” consist of monzodiorite, granodiorite and quartz monzonite that are classified as shoshonitic to high-K calc-alkaline series according to their chemical compositions. …”
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