Journal of Mineralogical and Petrological Sciences

Papers
(The H4-Index of Journal of Mineralogical and Petrological Sciences is 6. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2022-06-01 to 2026-06-01.)
ArticleCitations
New epidote-supergroup minerals from the Mogurazawa mine, Gunma, Japan: akasakaite-(Ce), akasakaite-(La), vanadoakasakaite-(Ce), and vanadoakasakaite-(La)12
K–Ar ages of volcanic rocks from the Himeshima volcanic group, northern Kyushu, Japan9
Zircon U-Pb ages of Cretaceous intrusive rocks in Central Yamaguchi, Southwest Japan: Implications for an enriched mantle source during a magmatic flare-up9
Prehnite-forming reactions in scapolite-bearing calc-silicate granulites from Rundvågshetta, Lützow-Holm Complex, East Antarctica7
Magma fractionation and emplacement mechanism in a subvolcanic plumbing system in a continental region: constraints from the late Neoproterozoic Wadi Dib ring complex in the Eastern Desert, Egypt7
Multiple post-peak metamorphic fluid infiltrations in southern Perlebandet, Sør Rondane Mountains, East Antarctica7
Petrogenesis of Josoji rhyolite and intrusive rocks of NE Shimane Peninsula, SW Japan: implication on Miocene volcanism related to back-arc rifting in San’in region6
High-K adakitic granite in post-Gondwana collisional stage: example for the Vengen Granite, Sør Rondane Mountains, East Antarctica6
Fluorescence spectroscopy of opal from the Shikaribetsu area, Shikaoi, Hokkaido6
The crystal chemistry of pumpellyite from Sugashima and julgoldite from Kouragahana, Japan: Toward a comprehensive understanding of the crystal chemistry of pumpellyite-group minerals6
Onboard measurements of the seismic velocity and electrical resistivity of dredged samples from the Southern Mariana region collected during cruise KH-23-96
New data on S-bearing katoite from Tadano, Fukushima Prefecture, Japan: an implication of the presence of both (SO<sub>3</sub>)<sup>2−</sup> and (SO<sub>4</sub>)<6
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