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  1. 1
    Faktor risiko penyakit berkaitan cara hidup di kalangan kakitangan kesihatan negeri Kelantan

    Faktor risiko penyakit berkaitan cara hidup di kalangan kakitangan kesihatan negeri Kelantan by Abu Hassan Shaari AK, Lila PMM, LetchumanGR, Ahmad Jusoh

    Published 2001
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  2. 2
    The potential of CO2 sequestration from basaltic rock in Peninsular Malaysia

    The potential of CO2 sequestration from basaltic rock in Peninsular Malaysia by Ahmad Fauzan Yusoff, Hijaz Kamal Hasnan, Muhammad Hatta Roselee, Khairul Azlan Mustapha, Azman Abdul Ghani

    Published 2025
    “…Both regions exhibit metaluminous properties that are compatible with a diverse range of mineral carbonation techniques. …”
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  3. 3
    Intraplate crustal remelting as the genesis of Jurassic high-K granites in the coastal region of the Guangdong Province, SE China

    Intraplate crustal remelting as the genesis of Jurassic high-K granites in the coastal region of the Guangdong Province, SE China by Huang, Hui-Qing, Li, X., Li, Zheng-Xiang, Li, W.

    Published 2013
    “…Instead, the group B granites, with features transitional between typical I-type and S-type granites, were most likely formed in a region where there was physical juxtaposition between infracrustal metaluminous and supracrustal peraluminous source rocks. …”
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  4. 4
    Response of zircon to melting and metamorphism in deep arc crust, Fiordland (New Zealand): implications for zircon inheritance in cordilleran granites

    Response of zircon to melting and metamorphism in deep arc crust, Fiordland (New Zealand): implications for zircon inheritance in cordilleran granites by Bhattacharya, S., Kemp, A., Collins, Bill

    Published 2018
    “…A comparison with lower- and upper-crustal, high Sr/Y metaluminous granites elsewhere in Fiordland shows that zircon inheritance is common in the deep crust, near the source region, but generally much less so in coeval, shallow magma chambers (plutons). …”
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  5. 5
    The oldest terrestrial mineral record: Thirty years of research on Hadean zircon from Jack Hills, Western Australia

    The oldest terrestrial mineral record: Thirty years of research on Hadean zircon from Jack Hills, Western Australia by Cavosie, Aaron, Valley, J., Wilde, S.

    Published 2018
    “…Trace element concentrations in Hadean grains (REE, Ti, Al, P, Y) are mostly similar to those in younger zircon from metaluminous granitoid generated at low magmatic temperatures, indicating consistent petrogenetic conditions. …”
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  6. 6
    On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China

    On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China by Li, X., Li, W., Li, Zheng-Xiang

    Published 2007
    “…The Early Yanshanian Nanling granitoid suites (including amphibole-bearing granodiorites->biotite monzogranites->K-feldspar granites->two-mica (muscovite) granites) are metaluminous to slightly peraluminous I-type or fractionated I-type granites. …”
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  7. 7
    Reactivation of the Archean lower crust: Implications for zircon geochronology, elemental and Sr–Nd–Hf isotopic geochemistry of late Mesozoic granitoids from northwestern Jiaodong Terrane, the North China Craton

    Reactivation of the Archean lower crust: Implications for zircon geochronology, elemental and Sr–Nd–Hf isotopic geochemistry of late Mesozoic granitoids from northwestern Jiaodong... by Yang, K., Fan, H., Santosh, M., Hu, F., Wilde, Simon, Lan, T., Lu, L., Liu, Y.

    Published 2012
    “…The rocks possess high CaO, TFe2O3 and MgO, and are metaluminous, with enrichment in LREEs and LILEs and depletion in HFSEs. …”
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  8. 8
    Early Permian post-collisional high-K granitoids from Liuyuan area in southern Beishan orogen, NW China: Petrogenesis and tectonic implications

    Early Permian post-collisional high-K granitoids from Liuyuan area in southern Beishan orogen, NW China: Petrogenesis and tectonic implications by Li, S., Wilde, Simon, Wang, T.

    Published 2013
    “…Early Permian granitic magmatism has been recognized from southern Beishan, NW China and they were emplaced between 275 Ma and 279 Ma according to LA-ICPMS zircon U–Pb dating. They are mainly metaluminous I-type and belong to the high-K calc-alkaline and shoshonitic series. …”
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  9. 9
    The Paleozoic northern margin of the Tarim Craton: Passive or active?

    The Paleozoic northern margin of the Tarim Craton: Passive or active? by Ge, Rongfeng, Zhu, W., Wu, H., Zheng, B., Zhu, X., He, J.

    Published 2012
    “…Geochemical data suggest that these granitoids are metaluminous, high K calc-alkaline granodiorite. They show a moderately differentiated REE pattern with insignificant Eu anomalies and are relatively depleted in Nb, Ta, Ti, P, but enriched in K and Ba, resembling Andean arc granite. …”
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  10. 10
    Geochronology, petrogenesis and tectonic implications of Triassic granitoids from Beishan, NW China

    Geochronology, petrogenesis and tectonic implications of Triassic granitoids from Beishan, NW China by Li, S., Wang, T., Wilde, Simon, Tong, Y., Hong, D., Guo, Q.

    Published 2012
    “…They belong to the high-K calc-alkaline and shoshonitic series and have alkalic and alkali-calcic characteristics, and are weakly peraluminous–metaluminous. These granitoids are mainly highly fractionated I-type granite and A-type granite. …”
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  11. 11
    Geochronology, petrogenesis and tectonic settings of pre- and syn-ore granites from the W-Mo deposits (East Kounrad, Zhanet and Akshatau), Central Kazakhstan

    Geochronology, petrogenesis and tectonic settings of pre- and syn-ore granites from the W-Mo deposits (East Kounrad, Zhanet and Akshatau), Central Kazakhstan by Li, G., Cao, M., Qin, K., Evans, Noreen, Hollings, P., Seitmuratova, E.

    Published 2016
    “…The pre-ore and ore-forming granites are high-K calc-alkaline, metaluminous to slightly peraluminous I-type granites. …”
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  12. 12
    Generation of Early Indosinian enriched mantle-derived granitoid pluton in the Sanjiang Orogen (SW China) in response to closure of the Paleo-Tethys

    Generation of Early Indosinian enriched mantle-derived granitoid pluton in the Sanjiang Orogen (SW China) in response to closure of the Paleo-Tethys by Zi, Jianwei, Cawood, P., Fan, W., Tohver, E., Wang, Y., McCuaig, T.

    Published 2012
    “…They display similar chemical and isotopic characteristics with a medium- to high-K, calc-alkaline, metaluminous I-type character, and similar whole rock Sr–Nd isotopic ratios, zircon εHf (t) (− 10 ± 1) and identical zircon δ18O (> 8‰ VSMOW). …”
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  13. 13
    Petrogenesis of the A-type, mesoproterozoic intra-caldera rheomorphic Kathleen Ignimbrite and Comagmatic Rowland suite intrusions, West Musgrave Province, Central Australia: Products of extreme fractional crystallization in a failed rift setting

    Petrogenesis of the A-type, mesoproterozoic intra-caldera rheomorphic Kathleen Ignimbrite and Comagmatic Rowland suite intrusions, West Musgrave Province, Central Australia: Produc... by Medlin, C., Jowitt, S., Cas, R., Smithies, R., Kirkland, Chris, Maas, R., Raveggi, M., Howard, H., Wingate, M.

    Published 2014
    “…These silicic rocks are A-type, metaluminous (to slightly peraluminous) rhyolites and are enriched in the rare earth elements (REE) relative to average crustal abundances. …”
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  14. 14
    Late Triassic melting of a thickened crust in southeastern China: Evidence for flat-slab subduction of the Paleo-Pacific plate

    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

    Published 2013
    “…In contrast to the west body, the east body has lower zircon saturation temperatures, lower whole-rock and zircon MREE/HREE ratios, higher Fe–Mg–Ti contents, and shows no depletion in Ba, Sr or Eu.The east body has higher magnetite contents, high magnetic susceptibilities and belongs to the magnetite-series. It is a metaluminous and magnesian granitoid of arc-affinity. …”
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  15. 15
    Tectono-magmatic evolution of Late Jurassic to Early Cretaceous granitoids in the west central Lhasa subterrane, Tibet

    Tectono-magmatic evolution of Late Jurassic to Early Cretaceous granitoids in the west central Lhasa subterrane, Tibet by Cao, M., Qin, K., Li, G., Li, J., Zhao, J., Evans, Noreen, Hollings, P.

    Published 2016
    “…We report whole rock geochemical and zircon U–Pb and Hf isotopic data for granitoids from the west central Lhasa subterrane (E80° to E86°). All rocks show metaluminous to peraluminous, calc-alkaline signatures, with strong depletion of Nb, Ta and Ti, enrichment of large ion lithophile elements (e.g., Cs, Rb, K), a negative correlation between SiO2 and P2O5, and a positive correlation between Rb and Th. …”
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  16. 16
    Petrology and geochemistry of the Teluk Ramunia volcanics, southeastern Johor,Peninsular Malaysia; implication for middle triassic tectonic / Muhammad Hatta Bin Roselee

    Petrology and geochemistry of the Teluk Ramunia volcanics, southeastern Johor,Peninsular Malaysia; implication for middle triassic tectonic / Muhammad Hatta Bin Roselee by Roselee, Muhammad Hatta

    Published 2014
    “…All rocks shows range from metaluminous to weakly peraluminous in term of their A/CNK value. …”
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  17. 17
    Constraining subduction-collision processes of the Paleo-Tethys along the Changning-Menglian Suture: New zircon U-Pb ages and Sr-Nd-Pb-Hf-O isotopes of the Lincang Batholith

    Constraining subduction-collision processes of the Paleo-Tethys along the Changning-Menglian Suture: New zircon U-Pb ages and Sr-Nd-Pb-Hf-O isotopes of the Lincang Batholith by Deng, J., Wang, C., Zi, Jianwei, Xia, R., Li, Q.

    Published 2017
    “…The Late Permian granodiorites are medium- to high-K calc-alkaline, metaluminous (A/CNK=0.99-1.10), with high Al 2 O 3 content (14.03wt%), high Mg # (46), high ( 87 Sr/ 86 Sr) i (0.7192-0.7278), negative whole-rock e Nd (t) (-14.7 to -8.5), ( 206 Pb/ 204 Pb) t of 18.199 to 18.791, ( 207 Pb/ 204 Pb) t of 15.714 to 15.765, ( 208 Pb/ 204 Pb) t of 38.500 to 38.851, zircon d 18 O SMOW =7.13‰-8.57‰, and zircon e Hf (t) of -14.8 to +0.4. …”
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  18. 18
    Age, composition, and source of continental arc- and syn-collision granites of the Neoproterozoic Sergipano Belt, Southern Borborema Province, Brazil

    Age, composition, and source of continental arc- and syn-collision granites of the Neoproterozoic Sergipano Belt, Southern Borborema Province, Brazil by Oliveira, E., Bueno, J., McNaughton, Neal, Silva Filho, A., Nascimento, R., Donatti-Filho, J.

    Published 2015
    “…These granitoids are dominantly high-K calc-alkaline, magnesian, metaluminous, mafic enclave-rich (Queimada Grande and Lajedinho), or with abundant inherited zircon grains (Poço Redondo and Sitios Novos). …”
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  19. 19
    Partial melting of thickened continental crust in central Tibet: Evidence from geochemistry and geochronology of Eocene adakitic rhyolites in the northern Qiangtang Terrane

    Partial melting of thickened continental crust in central Tibet: Evidence from geochemistry and geochronology of Eocene adakitic rhyolites in the northern Qiangtang Terrane by Long, X., Wilde, Simon, Wang, Q., Yuan, C., Wang, Xuan-Ce, Li, J., Jiang, Z., Dan, W.

    Published 2015
    “…In combination with data from previously-reported peraluminous and metaluminous adakitic rocks in the same region, the age and petrogenesis of the Suyingdi adakitic rhyolites suggest that the low-velocity zone in the deep crust of central and northern Tibet was most likely the result of partial melting of thickened crust.…”
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  20. 20
    Petrogenesis of the Cretaceous Zhangzhou batholith in southeastern China: Zircon U–Pb age and Sr–Nd–Hf–O isotopic evidence

    Petrogenesis of the Cretaceous Zhangzhou batholith in southeastern China: Zircon U–Pb age and Sr–Nd–Hf–O isotopic evidence by Chen, Jing-yuan, Yang, Jin-hui, Zhang, Ji-heng, Sun, Jin-feng, Wilde, Simon

    Published 2013
    “….%), with relatively homogeneous whole-rock initial 87Sr/86Sr ratios (~ 0.706), negative εNd(t) values of − 3.4 to − 2.7, chondrite-like εHf(t) values of − 0.3 to + 0.5, zircon εHf(t) values of − 0.8 to + 3.2 and δ18O values of + 5.0 to + 6.1‰, indicating that they were derived by partial melting of an enriched subcontinental lithospheric mantle, coupled with olivine and pyroxene fractionation.The calc-alkaline granodiorites and monzogranites are metaluminous and have relatively high SiO2 and low MgO contents. …”
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