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Renge Belt

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Journal Article
Published: 01 February 2005
Mineralogical Magazine (2005) 69 (1): 39–51.
...T. Morishita Abstract Coexisting Ba-rich (Cn 56–59 Or 40–42 Ab 2 An 0–1 ) and Ba-poor (Cn 7–15 Or 83–92 Ab 1–3 An 0–1 ) feldspars were found in a jadeitite collected from the Itoigawa-Ohmi district in the Renge high- P/T -type metamorphic belt, Japan. There is an apparent compositional gap...
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Journal Article
Published: 01 December 1997
Mineralogical Magazine (1997) 61 (6): 845–852.
Image
Geotectonic subdivision of Southwest Japan (modified from  Nishimiura, 1998...
Published: 01 November 2002
Fig. 1. Geotectonic subdivision of Southwest Japan (modified from Nishimiura, 1998 ). The Renge Belt is typically associated with meta-ophiolite sequences (470-340 Ma) including serpentinite. It is also characterized by association of glaucophane-schist.
Journal Article
Published: 01 February 2001
Mineralogical Magazine (2001) 65 (1): 111–120.
.... Renge near the locality and the Renge metamorphic belt where jadeitite deposits are found. \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \pagestyle{empty} \begin{document} \begin{eqnarray*}&&(Sr_{3.62}Ca_{0.08}Ce_...
FIGURES
Journal Article
Published: 01 November 2002
European Journal of Mineralogy (2002) 14 (6): 1119–1128.
...Fig. 1. Geotectonic subdivision of Southwest Japan (modified from Nishimiura, 1998 ). The Renge Belt is typically associated with meta-ophiolite sequences (470-340 Ma) including serpentinite. It is also characterized by association of glaucophane-schist. ...
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Image
Distribution of accretionary complexes, ancient arc systems and continental...
Published: 18 December 2018
Fig. 2. Distribution of accretionary complexes, ancient arc systems and continental fragments in Japan. HD: Hida Belt, OK: Oki Belt, HG: Hida Gaien Belt, OE: Oeyama Ophiolite, KS: Kurosegawa Belt, SK: South Kitakami Belt, ND: Nedamo Belt, NR: Renge Metamorphic Belt, AK: Akiyoshi Belt, SO: Suo
Image
Ocean plate stratigraphy of accretionary complexes of Japan, the age range ...
Published: 18 December 2018
: Nedamo Belt, C’: Renge metamorphic rocks, D: Akiyoshi Belt, E/E’: Suo Belt, F: Maizuru Belt, G: Ultra-Tamba Belt, H–K: Mino–Tamba Belt, Chichibu Belt and Ryoke Belt, I–J’: Ryoke Belt, K’: Sambagawa Belt, L: Northern Shimanto Belt, L’: Shimanto metamorphic rocks, M: Hidaka Belt, N: Southern Shimanto
Journal Article
Published: 18 December 2018
Geological Magazine (2021) 158 (1): 13–29.
...Fig. 2. Distribution of accretionary complexes, ancient arc systems and continental fragments in Japan. HD: Hida Belt, OK: Oki Belt, HG: Hida Gaien Belt, OE: Oeyama Ophiolite, KS: Kurosegawa Belt, SK: South Kitakami Belt, ND: Nedamo Belt, NR: Renge Metamorphic Belt, AK: Akiyoshi Belt, SO: Suo...
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Journal Article
Published: 15 March 2024
Journal of the Geological Society (2024) 181 (3): jgs2023-170.
... that integrates Permian accretionary tectonics at the convergence boundary with Triassic regional tectonics on the eastern margin of Asia. There are nine geological belts in western Japan – the Hida–Oki, Renge, Akiyoshi, Suo, Maizuru, Ultra-Tamba, Mino-Tamba, Ryoke and Chizu belts – along with the Nagato...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2016
DOI: 10.1144/GOJ.3
EISBN: 9781862397064
.... The geology of the Ryoke and Sanbagawa belts, the protoliths of which are ACs, is described in Chapter 2e. Renge high-P/T rocks (TT) Late Palaeozoic high-pressure and low-temperature (high- P/T ) metamorphic rocks known as the Renge metamorphic rocks were originally grouped within the so...
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Journal Article
Published: 01 January 2009
American Mineralogist (2009) 94 (1): 34–40.
... the Renge high- P / T metamorphic belt in the Itoigawa-Ohmi district of Japan. Morishita (2005) estimated a maximum metamorphic temperature of lower than 350°C. The present barian feldspar samples exhibit a very low albite content (2–4 mol%) (Fig. 7 ), similar to the result reported by Morishita (2005...
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Journal Article
Published: 01 March 2012
European Journal of Mineralogy (2012) 24 (2): 371–390.
... from the Osayama serpentinite melange, Sangun-Renge metamorphic belt, southwestern Japan . Mineral. Mag. , 61 , 845 – 852 . Tsujimori T. (2002) : Prograde and retrograde P-T paths of the late Paleozoic glaucophane eclogite from the Renge metamorphic belt, Hida Mountains, southwestern...
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Journal Article
Published: 01 December 2016
European Journal of Mineralogy (2016) 28 (6): 1029–1046.
... with Lws-BS-facies schists of the Renge belt ( Tsujimori & Itaya, 1999 ), and PrP-facies metamorphism in the Tobiishi sub-unit with that of BS/GS-facies schists of the Suo belt and/or PrP-facies rocks of the Mino-Tamba belt ( Nishimura, 1998 ) of the Inner Zone of Southwest Japan. These data support...
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Journal Article
Published: 01 January 2008
Journal of the Geological Society (2008) 165 (1): 221–234.
... (2005) in a jadeitite from the Itoigawa–Ohmi district in the Renge high- P – T metamorphic belt, Japan. Morishita implied that Ba-bearing fluids forming the jadeitite were possibly produced by dehydration of Ba-rich sediments in the early stages of subduction of oceanic crusts and could be related...
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Journal Article
Published: 01 August 2001
The Canadian Mineralogist (2001) 39 (4): 1199–1218.
... , 1686 . SrAl 2 Si 2 O 7 (OH) 2 ·H 2 O, orthorhombic, Cmcm The Sr-dominant analogue of lawsonite . Named after the discovery locality. Found at Oyashirazu, near Itoigawa Station, Itoigawa-Ohmi District, Niigata Prefecture, central Japan, in the Renge Belt, a classic locality of high-P...
Journal Article
Published: 01 September 2001
American Mineralogist (2001) 86 (9): 1112–1115.
... to high- P / T metamorphism. The new mineral name is for Mt. Renge, which is near the discovery locality and the jadeitite-bearing Renge metamorphic belt. Type material is in the Fossa Magna Museum at Itoigawa, and in the National Science Museum, Tokyo. J.L.J. S. Matsubara (2000) Vivianite...
Journal Article
Published: 01 January 2004
American Mineralogist (2004) 89 (1): 7–14.
... ) Omphacite-diopside vein in an omphacitite block from the Osayama serpentinite melange, Sangun-Renge metamorphic belt, southwestern Japan . Mineralogical Magazine , 61 , 845 – 852 . Tsujimori , T. ( 1998 ) Geology of the Osayama serpentinite melange in the central Chugoku Mountains...
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Journal Article
Published: 01 March 2012
European Journal of Mineralogy (2012) 24 (2): 237–246.
... feldspars in a jadeitite from the Itoigawa-Omi District in the Renge high-P/T-type metamorphic belt, Japan . Mineral. Mag. , 69 , 39 – 51 . Morley C.K. (2004) : Nested strike-slip duplexes, and other evidence for Late Cretaceous- Palaeogene transpressional tectonics before and during India...
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Journal Article
Journal: Geology
Published: 01 November 2013
Geology (2013) 41 (11): 1151–1154.
... stages and/or cycles in orogenic belts. Due to its considerable resistance to mechanical and chemical weathering, garnet is also commonly present as detrital grains in modern and ancient sediments. Therefore, some multistage garnets could potentially result from overgrowths on detrital grains. We report...
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Journal Article
Journal: Economic Geology
Published: 01 November 2019
Economic Geology (2019) 114 (7): 1467–1471.
... Mazaheri, Azadeh Malekzadeh Shafaroudi, and Minghua Ren article 106330 Stable isotope geochemistry of Chargar epithermal deposit: Constraints on epithermal systems in the Tarom metallogenic belt, NW Iran Seyed Hedayatalah Mousavi Motlagh, Majid Ghaderi, Narges Yasami, and Pura Alfonso article 106331...