- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Asia
-
Far East
-
Indonesia
-
Sunda Arc (1)
-
-
Japan
-
Hokkaido
-
Tokachi (1)
-
-
Honshu
-
Chiba Peninsula (1)
-
Chugoku (1)
-
Japanese Alps
-
Akaishi Mountains (1)
-
-
Kanto Mountains (1)
-
Kii Peninsula (2)
-
Kinki Japan (1)
-
Miura Peninsula (1)
-
Sagami Bay (1)
-
Tanzawa Mountains (1)
-
-
Honshu Arc (1)
-
Kyushu
-
Nagasaki Japan
-
Unzen (1)
-
-
Oita Japan
-
Beppu Japan (1)
-
Kuju (1)
-
-
-
Ryukyu Islands
-
Okinawa (1)
-
-
Shikoku (4)
-
Shimanto Belt (2)
-
-
Luzon Arc (1)
-
Philippine Islands
-
Luzon (3)
-
-
Taiwan
-
Chelungpu Fault (1)
-
Taipei Basin (1)
-
Taipei Taiwan (1)
-
Taiwanese Coastal Range (2)
-
-
-
Southeast Asia (3)
-
-
Australasia
-
Papua New Guinea (2)
-
-
NanTroSEIZE
-
Expedition 316
-
IODP Site C0007 (1)
-
-
Expedition 322 (1)
-
Expedition 333 (1)
-
IODP Site C0001 (1)
-
IODP Site C0002 (1)
-
IODP Site C0006 (1)
-
IODP Site C0011 (2)
-
IODP Site C0012 (2)
-
-
Oceania
-
Micronesia
-
Caroline Islands
-
Palau (1)
-
-
-
-
Pacific Ocean
-
North Pacific
-
Northwest Pacific
-
Celebes Sea (1)
-
East China Sea (1)
-
Izu-Bonin Arc (4)
-
Japan Sea
-
Oki Ridge (1)
-
-
Kumano Basin (1)
-
Mariana Trench (1)
-
Nankai Trough (7)
-
Okinawa Trough (1)
-
Philippine Sea
-
Daito Ridge (1)
-
Kyushu-Palau Ridge (1)
-
Ryukyu Trench (1)
-
West Philippine Basin (1)
-
-
Shikoku Basin (3)
-
South China Sea (2)
-
-
-
South Pacific
-
Southwest Pacific (2)
-
-
West Pacific
-
Banda Arc (1)
-
Indonesian Seas
-
Celebes Sea (1)
-
-
Northwest Pacific
-
Celebes Sea (1)
-
East China Sea (1)
-
Izu-Bonin Arc (4)
-
Japan Sea
-
Oki Ridge (1)
-
-
Kumano Basin (1)
-
Mariana Trench (1)
-
Nankai Trough (7)
-
Okinawa Trough (1)
-
Philippine Sea
-
Daito Ridge (1)
-
Kyushu-Palau Ridge (1)
-
Ryukyu Trench (1)
-
West Philippine Basin (1)
-
-
Shikoku Basin (3)
-
South China Sea (2)
-
-
Southwest Pacific (2)
-
-
-
West Pacific Ocean Islands
-
Bonin Islands (1)
-
-
-
commodities
-
geothermal energy (3)
-
metal ores
-
copper ores (3)
-
gold ores (2)
-
-
mineral deposits, genesis (2)
-
-
elements, isotopes
-
chemical ratios (1)
-
isotope ratios (4)
-
isotopes
-
radioactive isotopes
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (2)
-
-
stable isotopes
-
He-4/He-3 (1)
-
Nd-144/Nd-143 (1)
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (2)
-
Sr-87/Sr-86 (2)
-
-
-
metals
-
alkaline earth metals
-
magnesium (1)
-
strontium
-
Sr-87/Sr-86 (2)
-
-
-
hafnium (1)
-
lead
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (2)
-
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (1)
-
-
yttrium (1)
-
-
zirconium (1)
-
-
nitrogen (1)
-
noble gases
-
argon (1)
-
helium
-
He-4/He-3 (1)
-
-
-
-
fossils
-
Invertebrata
-
Protista
-
Radiolaria (1)
-
-
-
microfossils (1)
-
-
geochronology methods
-
Ar/Ar (2)
-
fission-track dating (5)
-
paleomagnetism (4)
-
thermochronology (1)
-
U/Pb (1)
-
-
geologic age
-
Cenozoic
-
Quaternary
-
Pleistocene (2)
-
-
Tertiary
-
Neogene
-
Miocene
-
lower Miocene (1)
-
upper Miocene (1)
-
-
Pliocene (2)
-
-
Paleogene
-
Eocene
-
middle Eocene (1)
-
-
-
-
-
Mesozoic (3)
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
ultramafics
-
peridotites
-
harzburgite (1)
-
-
-
-
porphyry (2)
-
volcanic rocks
-
adakites (2)
-
andesites
-
boninite (2)
-
-
basalts
-
tholeiite (1)
-
-
dacites (3)
-
rhyolites (1)
-
-
-
ophiolite (2)
-
-
metamorphic rocks
-
metamorphic rocks
-
metaigneous rocks
-
serpentinite (1)
-
-
metasedimentary rocks (2)
-
metasomatic rocks
-
serpentinite (1)
-
skarn (2)
-
-
-
ophiolite (2)
-
turbidite (1)
-
-
minerals
-
hydrates (1)
-
phosphates
-
apatite (1)
-
-
silicates
-
chain silicates
-
pyroxene group
-
clinopyroxene (1)
-
orthopyroxene (1)
-
-
-
orthosilicates
-
nesosilicates
-
olivine group
-
olivine (1)
-
-
zircon group
-
zircon (3)
-
-
-
-
sheet silicates
-
chlorite group
-
chlorite (1)
-
-
clay minerals
-
smectite (1)
-
-
illite (1)
-
-
-
-
Primary terms
-
absolute age (3)
-
Asia
-
Far East
-
Indonesia
-
Sunda Arc (1)
-
-
Japan
-
Hokkaido
-
Tokachi (1)
-
-
Honshu
-
Chiba Peninsula (1)
-
Chugoku (1)
-
Japanese Alps
-
Akaishi Mountains (1)
-
-
Kanto Mountains (1)
-
Kii Peninsula (2)
-
Kinki Japan (1)
-
Miura Peninsula (1)
-
Sagami Bay (1)
-
Tanzawa Mountains (1)
-
-
Honshu Arc (1)
-
Kyushu
-
Nagasaki Japan
-
Unzen (1)
-
-
Oita Japan
-
Beppu Japan (1)
-
Kuju (1)
-
-
-
Ryukyu Islands
-
Okinawa (1)
-
-
Shikoku (4)
-
Shimanto Belt (2)
-
-
Luzon Arc (1)
-
Philippine Islands
-
Luzon (3)
-
-
Taiwan
-
Chelungpu Fault (1)
-
Taipei Basin (1)
-
Taipei Taiwan (1)
-
Taiwanese Coastal Range (2)
-
-
-
Southeast Asia (3)
-
-
Australasia
-
Papua New Guinea (2)
-
-
Cenozoic
-
Quaternary
-
Pleistocene (2)
-
-
Tertiary
-
Neogene
-
Miocene
-
lower Miocene (1)
-
upper Miocene (1)
-
-
Pliocene (2)
-
-
Paleogene
-
Eocene
-
middle Eocene (1)
-
-
-
-
-
crust (13)
-
data processing (1)
-
Deep Sea Drilling Project
-
IPOD
-
Leg 58
-
DSDP Site 446 (1)
-
-
Leg 59
-
DSDP Site 447 (1)
-
-
-
Leg 31
-
DSDP Site 292 (1)
-
DSDP Site 294 (1)
-
-
-
deformation (3)
-
earthquakes (22)
-
engineering geology (1)
-
explosions (1)
-
faults (18)
-
geochemistry (3)
-
geochronology (3)
-
geodesy (1)
-
geomorphology (1)
-
geophysical methods (12)
-
geothermal energy (3)
-
heat flow (4)
-
igneous rocks
-
plutonic rocks
-
ultramafics
-
peridotites
-
harzburgite (1)
-
-
-
-
porphyry (2)
-
volcanic rocks
-
adakites (2)
-
andesites
-
boninite (2)
-
-
basalts
-
tholeiite (1)
-
-
dacites (3)
-
rhyolites (1)
-
-
-
Integrated Ocean Drilling Program
-
Expedition 316
-
IODP Site C0007 (1)
-
-
Expedition 322 (1)
-
Expedition 333 (1)
-
IODP Site C0001 (1)
-
IODP Site C0002 (1)
-
IODP Site C0006 (1)
-
IODP Site C0011 (2)
-
IODP Site C0012 (2)
-
-
intrusions (3)
-
Invertebrata
-
Protista
-
Radiolaria (1)
-
-
-
isostasy (1)
-
isotopes
-
radioactive isotopes
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (2)
-
-
stable isotopes
-
He-4/He-3 (1)
-
Nd-144/Nd-143 (1)
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (2)
-
Sr-87/Sr-86 (2)
-
-
-
lava (2)
-
magmas (3)
-
mantle (6)
-
Mesozoic (3)
-
metal ores
-
copper ores (3)
-
gold ores (2)
-
-
metals
-
alkaline earth metals
-
magnesium (1)
-
strontium
-
Sr-87/Sr-86 (2)
-
-
-
hafnium (1)
-
lead
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (2)
-
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (1)
-
-
yttrium (1)
-
-
zirconium (1)
-
-
metamorphic rocks
-
metaigneous rocks
-
serpentinite (1)
-
-
metasedimentary rocks (2)
-
metasomatic rocks
-
serpentinite (1)
-
skarn (2)
-
-
-
metasomatism (2)
-
mineral deposits, genesis (2)
-
Mohorovicic discontinuity (2)
-
nitrogen (1)
-
noble gases
-
argon (1)
-
helium
-
He-4/He-3 (1)
-
-
-
Ocean Drilling Program
-
Leg 190 (1)
-
Leg 195
-
ODP Site 1201 (1)
-
-
Leg 196 (1)
-
-
ocean floors (9)
-
Oceania
-
Micronesia
-
Caroline Islands
-
Palau (1)
-
-
-
-
orogeny (5)
-
Pacific Ocean
-
North Pacific
-
Northwest Pacific
-
Celebes Sea (1)
-
East China Sea (1)
-
Izu-Bonin Arc (4)
-
Japan Sea
-
Oki Ridge (1)
-
-
Kumano Basin (1)
-
Mariana Trench (1)
-
Nankai Trough (7)
-
Okinawa Trough (1)
-
Philippine Sea
-
Daito Ridge (1)
-
Kyushu-Palau Ridge (1)
-
Ryukyu Trench (1)
-
West Philippine Basin (1)
-
-
Shikoku Basin (3)
-
South China Sea (2)
-
-
-
South Pacific
-
Southwest Pacific (2)
-
-
West Pacific
-
Banda Arc (1)
-
Indonesian Seas
-
Celebes Sea (1)
-
-
Northwest Pacific
-
Celebes Sea (1)
-
East China Sea (1)
-
Izu-Bonin Arc (4)
-
Japan Sea
-
Oki Ridge (1)
-
-
Kumano Basin (1)
-
Mariana Trench (1)
-
Nankai Trough (7)
-
Okinawa Trough (1)
-
Philippine Sea
-
Daito Ridge (1)
-
Kyushu-Palau Ridge (1)
-
Ryukyu Trench (1)
-
West Philippine Basin (1)
-
-
Shikoku Basin (3)
-
South China Sea (2)
-
-
Southwest Pacific (2)
-
-
-
paleomagnetism (4)
-
plate tectonics (58)
-
sea-floor spreading (2)
-
sedimentary rocks
-
clastic rocks
-
sandstone (1)
-
-
-
sedimentation (2)
-
sediments
-
clastic sediments
-
alluvium (1)
-
mud (1)
-
sand (1)
-
-
marine sediments (1)
-
-
seismology (2)
-
soils (1)
-
stratigraphy (1)
-
structural analysis (1)
-
structural geology (1)
-
tectonics
-
neotectonics (4)
-
-
tectonophysics (4)
-
volcanology (2)
-
West Pacific Ocean Islands
-
Bonin Islands (1)
-
-
-
sedimentary rocks
-
sedimentary rocks
-
clastic rocks
-
sandstone (1)
-
-
-
turbidite (1)
-
volcaniclastics (1)
-
-
sediments
-
sediments
-
clastic sediments
-
alluvium (1)
-
mud (1)
-
sand (1)
-
-
marine sediments (1)
-
-
turbidite (1)
-
volcaniclastics (1)
-
-
soils
-
soils (1)
-
Philippine Sea Plate
Strain partitioning and interplate coupling along the northern margin of the Philippine Sea plate, estimated from Global Navigation Satellite System and Global Positioning System-Acoustic data
Scaling Relations of Earthquakes That Occurred in the Upper Part of the Philippine Sea Plate beneath the Kanto Region, Japan, Estimated by Means of Borehole Recordings
Moderate-magnitude seismicity remotely triggered in the Taiwan region by large earthquakes around the Philippine Sea plate
Paleomagnetic results from Palau, West Caroline Islands: A constraint on Philippine Sea plate motion
Subduction, bending and education; present and Quaternary tectonics of the northern border of the Philippine Sea Plate
Volcano-tectonic interactions during rapid plate-boundary evolution in the Kyushu region, SW Japan
The relationships between mountain building, surface erosion, sediment supply to the trench, and growth of the accretionary prism are examined in southwest Japan and the Nankai Trough. Mountain building caused by the subduction of the Philippine Sea plate in the Nankai Trough and collision in central Japan has resulted in a rock uplift rate of ∼4 mm/yr. Surface denudation rates in the mountain regions are on the order of 3–4 mm/yr, resulting from the heavy rainfall of the Asian monsoon. This fact suggests that mountain building is almost in an equilibrium stage in which surface erosion and rock uplift balance each other, resulting in a constant altitude of ∼2000 m. Several drainage systems on land and in offshore submarine canyons enable the transport of eroded sediments directly into the Nankai Trough. Most of the terrigenous sediments supplied to the Nankai Trough are accreted in the subduction zone of the Philippine Sea plate. The accretion rate of the sediments in the eastern Nankai Trough is ∼1.68 × 10 7 m 3 /yr, which is consistent with the denudation rate of the Akaishi Mountains, contributing to the supply of 1.72 × 10 7 m 3 /yr of sediment in central Japan. The growth of the accretionary prism is an important controlling factor for the onset of large earthquakes in the Nankai Trough, because the hanging wall of the rupture area of the seismogenic zone is composed entirely of the accretionary prism. Repeated large earthquakes with a recurrence time of ∼100–200 yr, which are well recorded in the Nankai Trough, in turn promote surface erosion through consecutive landslides and tsunamis. Southwest Japan, with its extensive record of both erosional processes and seismic events, shows the intimate long-term relationships between tectonically driven mountain building, surface erosion under the Asian monsoon climate, growth of the accretionary prism in the trench, and the generation of large earthquakes.
Origin and geodynamic implication of the Dupal isotopic anomaly in volcanic rocks from the Philippine island arcs
Difference in N 2 /Ar ratio of magmatic gases from northeast and southwest Japan: New evidence for different states of plate subduction
A New Ground‐Motion Prediction Equation of Japanese Instrumental Seismic Intensities Reflecting Source Type Characteristics in Japan
ABSTRACT Understanding the factors controlling earthquake rupture areas in subduction zones is a fundamental question in geodynamic research. In the Nankai Trough, Japan, three major controlling factors have been proposed so far: surface roughness, such as seamounts, on the subducting Philippine Sea plate, a locally dense and rigid upper plate, and stable or unstable frictional properties of the plate-boundary megathrust with abnormal pore-fluid pressure. The most prominent rupture segment boundary in the Nankai Trough is located off the Kii Peninsula. When the rupture starts and propagates beyond this boundary, the entire megathrust breaks, as in the 1707 Hoei earthquake. When the rupture does not propagate beyond this portion, the rupture area is segmented, as in the 1854 Ansei, 1944 Tonankai, and 1946 Nankai earthquakes. In this case, the boundary works as a barrier. The asperity or barrier depends on the frictional behavior along the megathrust in this area. Thick and dense plutonic rocks are the main component of the upper plate of the Kii Peninsula. Magmatic activity associated with the proto–Izu-Bonin arc collision is speculated to have occurred in the middle Miocene. Thus, we propose that the long-term tectonic hysteresis of the upper plate is the main factor controlling the rupture area segmentation in the Nankai Trough.