1-20 OF 460 RESULTS FOR

Miyazaki Group

Results shown limited to content with bounding coordinates.
Save search
Follow your search
Access your saved searches in your account
Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article

Pteropods (Mollusca, Gastropoda) from the Pliocene Miyazaki Group, Miyazaki Prefecture, Japan Free

Atsushi Ujihara
Published: 01 September 1996
Journal of Paleontology (1996) 70 (5): 771–788.
Add to Citation Manager for Pteropods (Mollusca, Gastropoda) from the Pliocene <span class="search-highlight">Miyazaki</span> <span class="search-highlight">Group</span>, <span class="search-highlight">Miyazaki</span> Prefecture, Japan
Image
Index map and distribution of the Miyazaki Group (Nakamura et al. 1999). A) The Miyazaki Group is distributed near Miyazaki in Miyazaki Prefecture, SW Japan. B) A tuff, B tuff, and C tuff of the key tuff bed are indicated.

Index map and distribution of the Miyazaki Group ( Nakamura et al. 1999 ). ... Available to Purchase

Published: 20 February 2018
Fig. 1.— Index map and distribution of the Miyazaki Group ( Nakamura et al. 1999 ). A) The Miyazaki Group is distributed near Miyazaki in Miyazaki Prefecture, SW Japan. B) A tuff, B tuff, and C tuff of the key tuff bed are indicated.
Image
Stratigraphic columns of the Miyazaki Group (after Nakamura et al. 1999).

Stratigraphic columns of the Miyazaki Group (after Nakamura et al. 1999 ).... Available to Purchase

Published: 20 February 2018
Fig. 3.— Stratigraphic columns of the Miyazaki Group (after Nakamura et al. 1999 ).
Image
A) Locality of the Nichinan Coast. B) Geological map of the southern part of the Miyazaki Group. C) Localities of studied sections. Studied sections (A, K, and I sections) along the Nichinan Coast, were correlated using key tuff maker beds (A, B, and C. Part B modified from Nakamura et al. 1999; Onishi et al. 2018).

A) Locality of the Nichinan Coast. B) Geological map of the southern par... Available to Purchase

Published: 11 May 2024
Fig. 1. A) Locality of the Nichinan Coast. B) Geological map of the southern part of the Miyazaki Group. C) Localities of studied sections. Studied sections (A, K, and I sections) along the Nichinan Coast, were correlated using key tuff maker beds (A, B, and C. Part B modified from
Journal Article

Facies Distribution in Sediment-gravity-flow Deposits Constructing Sediment Waves: an Outcrop Example of Forearc Basin Fills, Neogene Aoshima Formation, Southwest Japan Available to Purchase

Yuri Onishi, Kiwako Takii-Kawakami, Hiroko Abe, Yoshiro Ishihara
Published: 20 February 2018
Journal of Sedimentary Research (2018) 88 (2): 260–275.
DOI: https://doi.org/10.2110/jsr.2018.6
...Fig. 1.— Index map and distribution of the Miyazaki Group ( Nakamura et al. 1999 ). A) The Miyazaki Group is distributed near Miyazaki in Miyazaki Prefecture, SW Japan. B) A tuff, B tuff, and C tuff of the key tuff bed are indicated. ...
FIGURES | View All (14)
View PDF for article title, Facies Distribution in Sediment-gravity-flow Deposits Constructing Sediment Waves: an Outcrop Example of Forearc Basin Fills, Neogene Aoshima Formation, Southwest Japan
Purchase
Add to Citation Manager for Facies Distribution in Sediment-gravity-flow Deposits Constructing Sediment Waves: an Outcrop Example of Forearc Basin Fills, Neogene Aoshima Formation, Southwest Japan
Journal Article

Random and time-persistent depositional processes in turbidite successions: an example from the marine deep-water Aoshima Formation (Neogene, Kyushu Island, southwest Japan) Available to Purchase

Yoshiro Ishihara, Keisuke Kimata, Yuri Onishi
Published: 11 May 2024
Journal of Sedimentary Research (2024) 94 (3): 251–265.
DOI: https://doi.org/10.2110/jsr.2022.067
...Fig. 1. A) Locality of the Nichinan Coast. B) Geological map of the southern part of the Miyazaki Group. C) Localities of studied sections. Studied sections (A, K, and I sections) along the Nichinan Coast, were correlated using key tuff maker beds (A, B, and C. Part B modified from...
FIGURES | View All (11)
View PDF for article title, Random and time-persistent depositional processes in turbidite successions: an example from the marine deep-water Aoshima Formation (Neogene, Kyushu Island, southwest Japan)
Purchase
Add to Citation Manager for Random and time-persistent depositional processes in turbidite successions: an example from the marine deep-water Aoshima Formation (Neogene, Kyushu Island, southwest Japan)
Includes: Supplemental Content
Image
Relationship between R2mean and 1σ within a single sample. Data are divided into different groups representing the sample positions in the metamorphic zones proposed by Miyazaki et al. [22].

Relationship between R2 mean and 1 σ within a single sample. Data a... Open Access

Published: 08 April 2022
Figure 5 Relationship between R2 mean and 1 σ within a single sample. Data are divided into different groups representing the sample positions in the metamorphic zones proposed by Miyazaki et al. [ 22 ].
Image
CORRECTED VERSION Map of the study area. The gray lines mark the seismic profiles acquired across the region, and the white lines indicate profiles that are presented as figures. The red circles mark the boreholes in the study region. The white circles mark active fluid vents; the location of the Yaeyama Knoll is from Miyazaki et al. (2017) and the locations of the others are from Ishibashi et al. (2015). cbvt = cross-backarc volcanic trail; CSU = Changshu uplift; DBS = Diaobei sag; ECSSB = East China Sea Shelf Basin; EDG = East Depression group; FJS = Fujiang sag; FZS = Fuzhou sag; HJU = Haijiao uplift; HPJU = Hupijiao uplift; JJS = Jiaojiang sag; JSBU = Jinshanbei uplift; JSNS = Jinshannan sag; KSS = Kunshan sag; LSS = Lishui sag; OT = Okinawa Trough; PJYS = Pengjiayu sag; QTS = Qiantang sag; vamp = volcanic arc migration phenomenon; WDG = West Depression group; XHS = Xihu sag; YDU = Yandang uplift; YSDU = Yushandong uplift.

CORRECTED VERSION Map of the study area. The gray lines mark the seismic pr... Available to Purchase

Published: 01 March 2023
; the location of the Yaeyama Knoll is from Miyazaki et al. (2017) and the locations of the others are from Ishibashi et al. (2015) . cbvt = cross-backarc volcanic trail; CSU = Changshu uplift; DBS = Diaobei sag; ECSSB = East China Sea Shelf Basin; EDG = East Depression group; FJS = Fujiang sag; FZS = Fuzhou
Image
Upper two diagrams. R2max (vertical axis) versus horizontal distance (horizontal axis) from contacts with (a) the Shinshiro tonalite and (b) the Busetsu granite. Lower two diagrams. Peak temperature estimated using RSCM thermometry (vertical axis) versus horizontal distance (horizontal axis) from contacts with (c) the Shinshiro tonalite and (d) the Busetsu granite. In (b) and (d), data&lt;5 km from the Shinshiro tonalite are excluded. The data are separated into different groups corresponding to the location of the samples within the metamorphic zonation proposed by Miyazaki et al. [22]. The two data shown by white diamonds contain only graphite, and the estimated temperature is a minimum. The symbols shown with a red border indicate that the mean value has been corrected by excluding values for detrital CM. The distance represents the closest distance between the sample location and the outlines of the relevant pluton calculated using a geological map (Figure 2) and QGIS 3.0.

Upper two diagrams. R2 max (vertical axis) versus horizontal distance (hor... Open Access

Published: 08 April 2022
axis) from contacts with (c) the Shinshiro tonalite and (d) the Busetsu granite. In (b) and (d), data < 5   km from the Shinshiro tonalite are excluded. The data are separated into different groups corresponding to the location of the samples within the metamorphic zonation proposed
Book Chapter

Neogene–Quaternary sedimentary successions Available to Purchase

Author(s)
Makoto Ito, Koji Kameo, Yasufumi Satoguchi, Fujio Masuda, Yoshihisa Hiroki, Osamu Takano, Takeshi Nakajima, Noriyuki Suzuki
Book: The Geology of Japan
Series: Geological Society, London, Geology of Series
Publisher: The Geological Society of London
Published: 01 January 2016
DOI: 10.1144/GOJ.12
EISBN: 9781862397064
.... For example, while more than 300 tephras have been described from the Kazusa Group on the Boso Peninsula, only 28 of them have been correlated with tephras elsewhere. Furthermore, some areas have few widespread tephras useful for the regional correlation. This is the case in the Miyazaki Group in the Miyazaki...
FIGURES | View All (20)
Abstract
View PDF for content titled, Neogene–Quaternary sedimentary successions
Purchase
Add to Citation Manager for Neogene–Quaternary sedimentary successions

Abstract Neogene and Quaternary sedimentary successions are widely distributed across the Japanese islands, commonly underlying or distributing nearby heavily populated areas where the infrastructure of Japanese society is fully developed. Furthermore, some Neogene sedimentary successions contain oil and gas and have played an important role in hydrocarbon production in Japan. The Neogene and Quaternary sedimentary basins formed as a response to the development of the Japanese arc-trench system as a result of the opening of the Sea of Japan (c. 15 Ma), and spatial and temporal variations in the sedimentary successions are considered to have been controlled by the interaction between glacial-interglacial sea-level changes and active tectonic movements of the arc-trench system, which has been controlled mainly by subduction of the Paci?c and Philippine Sea plates beneath the Japanese islands.

Journal Article

Nanshanophyllum and Shensiphyllum (Silurian Rugosa) from the Kurosegawa Terrane, Southwest Japan, and Their Paleobiogeographic Implications Available to Purchase

Erika Kido
Published: 01 March 2009
Journal of Paleontology (2009) 83 (2): 280–292.
DOI: https://doi.org/10.1666/08-113.1
..., Daguan, Yunnan, China ( Chen et al., 2005 ). Stereoxylodes bailongjiangensis Cao; Upper Llandovery of the Zhugqu Group, Zhugqu, Gansu, China ( Cao and Lin, 1982 ). Nanshanophyllum hamadai n. sp.; Upper Llandovery of the Middle Member of the Gionyama Formation, Mt. Gionyama, Miyazaki...
FIGURES | View All (12)
View PDF for article title, Nanshanophyllum and Shensiphyllum (Silurian Rugosa) from the Kurosegawa Terrane, Southwest Japan, and Their Paleobiogeographic Implications
Purchase
Add to Citation Manager for Nanshanophyllum and Shensiphyllum (Silurian Rugosa) from the Kurosegawa Terrane, Southwest Japan, and Their Paleobiogeographic Implications
Journal Article

Contact metamorphism of a Cretaceous accretionary prism by the 14 Ma Okueyama granite, a single post-kinematic pluton in Central Kyushu, Japan: SVD analysis of metamorphic reactions and thermal release Available to Purchase

Takashi Yuguchi, Tomoyuki Miyazoe, Tadao Nishiyama
Published: 01 February 2011
American Mineralogist (2011) 96 (2-3): 308–318.
DOI: https://doi.org/10.2138/am.2011.3445
... of an accretionary prism is a key factor in understanding the nature of a Pacific-type orogeny. Miyazaki and Okumura (2002) discussed low P-T metamorphism (prehnite-actinolite facies) in the Shimanto Accretionary Complex in Kyushu (the Cretaceous Makimine Formation in the Lower Shimanto Group) based...
FIGURES | View All (6)
View PDF for article title, Contact metamorphism of a Cretaceous accretionary prism by the 14 Ma Okueyama granite, a single post-kinematic pluton in Central Kyushu, Japan: SVD analysis of metamorphic reactions and thermal release
Purchase
Add to Citation Manager for Contact metamorphism of a Cretaceous accretionary prism by the 14 Ma Okueyama granite, a single post-kinematic pluton in Central Kyushu, Japan: SVD analysis of metamorphic reactions and thermal release
Journal Article

SILURIAN RUGOSE CORALS FROM THE KUROSEGAWA TERRANE, SOUTHWEST JAPAN, AND THE FIRST OCCURRENCE OF NEOBRACHYELASMA Available to Purchase

ERIKA KIDO
Published: 01 May 2010
Journal of Paleontology (2010) 84 (3): 466–476.
DOI: https://doi.org/10.1666/09-037.1
... the Silurian of the South Kitakami Terrane (Northeast Japan) by Kato et al. (1980) and Kawamura (1983) . Amplexoides was listed by Kato et al. (1980) , without description, from the Silurian of the Fukata Formation of the Yokokurayama Group, which is assigned to the Kurosegawa Terrane. The specimens...
FIGURES | View All (9)
View PDF for article title, SILURIAN RUGOSE CORALS FROM THE KUROSEGAWA TERRANE, SOUTHWEST JAPAN, AND THE FIRST OCCURRENCE OF NEOBRACHYELASMA
Purchase
Add to Citation Manager for SILURIAN RUGOSE CORALS FROM THE KUROSEGAWA TERRANE, SOUTHWEST JAPAN, AND THE FIRST OCCURRENCE OF NEOBRACHYELASMA
Journal Article

2024 Thematic Preview Free

Journal: Elements
Published: 01 December 2023
Elements (2023) 19 (6): 338–339.
DOI: https://doi.org/10.2138/gselements.19.6.338
...) PAIRED METAMORPHIC BELTS OF SW JAPAN: METAMORPHIC RECORDS OF A SUBDUCTION SYSTEM Guest Editors: S. R. Wallis (University of Tokyo, Japan), K. Miyazaki (Geological Survey of Japan, AIST, Japan), and U. Knittel (RWTH Aachen University, Germany) Subduction, where one plate dives beneath another, controls...
View PDF for article title, 2024 Thematic Preview
Add to Citation Manager for 2024 Thematic Preview
Journal Article

Anisotropic growth of olivine during crystallization in basalts from Hawaii: Implications for olivine fabric development Available to Purchase

Da-Peng Wen, Yong-Feng Wang, Jun-Feng Zhang, Zhen-Min Jin
Published: 01 May 2018
American Mineralogist (2018) 103 (5): 735–741.
DOI: https://doi.org/10.2138/am-2018-6174
... observations suggest that, although differing in growth environments (for instance, free space, available constituents, etc.), olivine growth under subsolidus conditions is also anisotropic (e.g., Drury and van Roermund 1989 ; Tommasi et al. 2008 ; Miyazaki et al. 2013 ). Nevertheless, the growth habits...
FIGURES | View All (5)
View PDF for article title, Anisotropic growth of olivine during crystallization in basalts from Hawaii: Implications for olivine fabric development
Purchase
Add to Citation Manager for Anisotropic growth of olivine during crystallization in basalts from Hawaii: Implications for olivine fabric development
Journal Article

Crustal Deformation Associated with the 2011 Tohoku-Oki Earthquake: An Overview Available to Purchase

Manabu Hashimoto
Published: 01 March 2013
Earthquake Spectra (2013) 29 (1_suppl): 81–98.
DOI: https://doi.org/10.1193/1.4000117
.... Open stars are the epicenter of large aftershocks and induced events. Thick solid lines show major rivers. K.R. denotes the Kitakami River. A line with barb is the axis of Japan Trench ( Bird 2003 ). Several groups tried to invert interseismic GPS deformation data and obtained the distribution...
FIGURES | View All (12)
View PDF for article title, Crustal Deformation Associated with the 2011 Tohoku-Oki Earthquake: An Overview
Purchase
Add to Citation Manager for Crustal Deformation Associated with the 2011 Tohoku-Oki Earthquake: An Overview
Journal Article

Recognition of Detrital Carbonaceous Material in the Ryoke Metamorphic Belt by Using Raman Thermometry: Implications for Thermal Structure and Detrital Origin Open Access

Ken Yamaoka, Simon R. Wallis, Akira Miyake, Yui Kouketsu
Journal: Lithosphere
Publisher: GSW
Published: 08 April 2022
Lithosphere (2022) 2022 (1): 3899340.
DOI: https://doi.org/10.2113/2022/3899340
...Figure 5 Relationship between R2 mean and 1 σ within a single sample. Data are divided into different groups representing the sample positions in the metamorphic zones proposed by Miyazaki et al. [ 22 ]. ...
FIGURES | View All (10)
View PDF for article title, Recognition of Detrital Carbonaceous Material in the Ryoke Metamorphic Belt by Using Raman Thermometry: Implications for Thermal Structure and Detrital Origin
Add to Citation Manager for Recognition of Detrital Carbonaceous Material in the Ryoke Metamorphic Belt by Using Raman Thermometry: Implications for Thermal Structure and Detrital Origin
Includes: Supplemental Content
Journal Article

MINERALOGICAL AND OXYGEN ISOTOPIC CONSTRAINTS ON THE ORIGIN OF THE CONTACT-METAMORPHOSED BEDDED MANGANESE DEPOSIT AT NAGASAWA, JAPAN Available to Purchase

Makoto Haruna, Hisao Satoh, Yasuyuki Banno, Masahide Kono, Michiaki Bunno
Published: 01 August 2002
The Canadian Mineralogist (2002) 40 (4): 1069–1089.
DOI: https://doi.org/10.2113/gscanmin.40.4.1069
... volcanosedimentary sequences, e.g., in the Franciscan Complex in California ( e.g., Hein et al. 1987 , Hein & Koski 1987 , Huebner & Flohr 1990 ), in the Gambatesa district in eastern Liguria ( Marescotti & Frezzotti 2000 ), in the Proterozoic Vittinki Group in Finland ( Mancini et al. 2000...
FIGURES | View All (12)
View PDF for article title, MINERALOGICAL AND OXYGEN ISOTOPIC CONSTRAINTS ON THE ORIGIN OF THE CONTACT-METAMORPHOSED BEDDED MANGANESE DEPOSIT AT NAGASAWA, JAPAN
Purchase
Add to Citation Manager for MINERALOGICAL AND OXYGEN ISOTOPIC CONSTRAINTS ON THE ORIGIN OF THE CONTACT-METAMORPHOSED BEDDED MANGANESE DEPOSIT AT NAGASAWA, JAPAN
Journal Article

A Method for Rapid Estimation of Moment Magnitude for Early Tsunami Warning Based on Coastal GPS Networks Available to Purchase

S. K. Singh, X. Pérez-Campos, A. Iglesias, D. Melgar
Published: 01 May 2012
Seismological Research Letters (2012) 83 (3): 516–530.
DOI: https://doi.org/10.1785/gssrl.83.3.516
... waveforms have been used in many studies to map slip on the fault. Since continuous GPS data provide displacement seismograms, this has opened the new field of GPS seismology ( e.g. , Nikolaidis et al. 2001 ; Larson et al. 2003 ; Bock et al. 2004 ; Miyazaki et al. 2004 ). Advantages of GPS...
FIGURES | View All (11)
View PDF for article title, A Method for Rapid Estimation of Moment Magnitude for Early Tsunami Warning Based on Coastal GPS Networks
Purchase
Add to Citation Manager for A Method for Rapid Estimation of Moment Magnitude for Early Tsunami Warning Based on Coastal GPS Networks
Book Chapter

The Kyushu–Ryukyu Arc Available to Purchase

Author(s)
Kazuhiro Miyazaki, Masaki Ozaki, Makoto Saito, Seiichi Toshimitsu
Book: The Geology of Japan
Series: Geological Society, London, Geology of Series
Publisher: The Geological Society of London
Published: 01 January 2016
DOI: 10.1144/GOJ.6
EISBN: 9781862397064
... and hot plate (Miyazaki & Okumura 2002). Metamorphic ages of the Morotsuka Group are estimated to be 60-50 Ma based on muscovite K-Ar data from meta-mudstone (Hara & Kimura 2008) and K-feldspar K-Ar data from sandstones ( Teraoka et al. 1994 ) of the Kamae Subgroup. Finally, in Okinawajima...
FIGURES | View All (26)
Abstract
View PDF for content titled, The Kyushu–Ryukyu Arc
Purchase
Add to Citation Manager for The Kyushu–Ryukyu Arc

Abstract The Kyushu-Ryukyu Arc extends for over 1000 km south from the large island of Kyushu down the Ryukyu Island chain towards Taiwan. It has been produced by subduction of oceanic plates beneath the Eurasian continent and exposes a wide range of Palaeozoic, Mesozoic and Cenozoic rocks formed in an active continental margin setting (Maruyama et al. 1997; Isozaki et al. 2010). In this chapter we describe the geology of the arc from the oldest (Palaeozoic and Triassic) to youngest (Neogene and Quaternary) rocks, and discuss the geodynamic evolution of the area.