- 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
-
China
-
Guizhou China (1)
-
Hebei China
-
Tianjin China (1)
-
-
Jilin China (1)
-
Sichuan China (2)
-
Songliao Basin (1)
-
Xizang China
-
Gangdese Belt (1)
-
Lhasa Block (3)
-
-
Yunnan China (1)
-
-
-
Tibetan Plateau (2)
-
-
Pacific Ocean
-
East Pacific
-
Northeast Pacific (1)
-
-
North Pacific
-
Northeast Pacific (1)
-
-
-
Santa Maria Basin (1)
-
United States
-
California (1)
-
Texas
-
Fort Worth Basin (1)
-
-
-
-
commodities
-
petroleum
-
natural gas
-
shale gas (1)
-
-
shale oil (1)
-
-
water resources (1)
-
-
elements, isotopes
-
carbon
-
organic carbon (1)
-
-
isotope ratios (3)
-
isotopes
-
stable isotopes
-
Hf-177/Hf-176 (3)
-
Nd-144/Nd-143 (2)
-
Sr-87/Sr-86 (2)
-
-
-
metals
-
alkaline earth metals
-
strontium
-
Sr-87/Sr-86 (2)
-
-
-
hafnium
-
Hf-177/Hf-176 (3)
-
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (2)
-
-
-
titanium (1)
-
-
-
geochronology methods
-
U/Pb (4)
-
-
geologic age
-
Cenozoic
-
Tertiary
-
Paleogene
-
Eocene (1)
-
Oligocene (1)
-
-
-
-
Mesozoic
-
Cretaceous
-
Upper Cretaceous (1)
-
-
Jurassic (1)
-
Triassic
-
Upper Triassic (1)
-
-
-
Paleozoic
-
Carboniferous
-
Mississippian
-
Barnett Shale (1)
-
-
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
granites
-
monzogranite (1)
-
-
-
volcanic rocks
-
glasses (1)
-
rhyolites (1)
-
-
-
-
metamorphic rocks
-
metamorphic rocks
-
gneisses
-
orthogneiss (1)
-
-
-
-
minerals
-
oxides
-
magnesium oxides (1)
-
-
phosphates
-
apatite (1)
-
-
silicates
-
framework silicates
-
silica minerals
-
quartz (1)
-
-
-
orthosilicates
-
nesosilicates
-
zircon group
-
zircon (4)
-
-
-
-
-
-
Primary terms
-
absolute age (4)
-
Asia
-
Far East
-
China
-
Guizhou China (1)
-
Hebei China
-
Tianjin China (1)
-
-
Jilin China (1)
-
Sichuan China (2)
-
Songliao Basin (1)
-
Xizang China
-
Gangdese Belt (1)
-
Lhasa Block (3)
-
-
Yunnan China (1)
-
-
-
Tibetan Plateau (2)
-
-
carbon
-
organic carbon (1)
-
-
Cenozoic
-
Tertiary
-
Paleogene
-
Eocene (1)
-
Oligocene (1)
-
-
-
-
fractures (1)
-
geophysical methods (2)
-
ground water (1)
-
igneous rocks
-
plutonic rocks
-
granites
-
monzogranite (1)
-
-
-
volcanic rocks
-
glasses (1)
-
rhyolites (1)
-
-
-
intrusions (1)
-
isotopes
-
stable isotopes
-
Hf-177/Hf-176 (3)
-
Nd-144/Nd-143 (2)
-
Sr-87/Sr-86 (2)
-
-
-
land subsidence (1)
-
land use (1)
-
magmas (2)
-
mantle (1)
-
Mesozoic
-
Cretaceous
-
Upper Cretaceous (1)
-
-
Jurassic (1)
-
Triassic
-
Upper Triassic (1)
-
-
-
metals
-
alkaline earth metals
-
strontium
-
Sr-87/Sr-86 (2)
-
-
-
hafnium
-
Hf-177/Hf-176 (3)
-
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (2)
-
-
-
titanium (1)
-
-
metamorphic rocks
-
gneisses
-
orthogneiss (1)
-
-
-
Pacific Ocean
-
East Pacific
-
Northeast Pacific (1)
-
-
North Pacific
-
Northeast Pacific (1)
-
-
-
Paleozoic
-
Carboniferous
-
Mississippian
-
Barnett Shale (1)
-
-
-
-
petroleum
-
natural gas
-
shale gas (1)
-
-
shale oil (1)
-
-
plate tectonics (1)
-
remote sensing (1)
-
sedimentary rocks
-
clastic rocks
-
shale (1)
-
-
-
slope stability (2)
-
United States
-
California (1)
-
Texas
-
Fort Worth Basin (1)
-
-
-
water resources (1)
-
-
rock formations
-
Monterey Formation (1)
-
-
sedimentary rocks
-
sedimentary rocks
-
clastic rocks
-
shale (1)
-
-
-
Compositional change from high-Mg to low-Mg magmatism at ca. 150 Ma in the central Lhasa terrane, Tibet: Switching from advancing to retreating subduction of the Bangong Tethyan slab
Analysis of Temporal and Spatial Evolution Characteristics of Land Subsidence in Western Songnen Plain Using Multisource Remote Sensing
Origin of Tibetan post-collisional high-K adakitic granites: Anatexis of intermediate to felsic arc rocks
Cumulate granites: A perspective from new apatite MgO partition coefficients
Imaging the Late Triassic lithospheric architecture of the Yidun Terrane, eastern Tibetan Plateau: Observations and interpretations
Reheating and Magma Mixing Recorded by Zircon and Quartz from High-Silica Rhyolite in the Coqen Region, Southern Tibet
Abstract A compilation of 290 zircon U–Pb ages of intrusive rocks indicates that the Gangdese Batholith in southern Tibet was emplaced from c. 210 Ma to c. 10 Ma. Two intense magmatic pulses within the batholith occur at: (1) 90 ± 5 Ma, which is restricted to 89–94° E in the eastern segment of the southern Lhasa subterrane; and (2) 50 ± 3 Ma, which is widespread across the entire southern Lhasa subterrane. The latter pulse was followed by a phase of widespread but volumetrically small, dominantly felsic adakitic intrusive rocks at 16 ± 2 Ma. The Linzizong volcanism in the Linzhou Basin was active from 60.2 to 52.3 Ma, rather than 69–44 Ma as previously estimated. During 120–75 Ma, Gangdese Batholith magmatism migrated from south to north, arguing against rollback of the downgoing, north-dipping Neo-Tethyan oceanic lithosphere for the generation of the 90 ± 5 Ma magmatic pulse. Petrological, geochemical and metamorphic data indicate that this pulse was likely to have been generated through subduction of the Neo-Tethyan oceanic ridge lithosphere. Subsequent Gangdese Batholith magmatism propagated both south and north during 70–45 Ma, and finally concentrated at the southern margin of the Lhasa Terrane at 45–30 Ma. The enhanced mafic magmatism since c. 70 Ma, magmatic flare-up with compositional diversity at c. 51 Ma and increased magmatic temperature at 52–50 Ma are interpreted as the consequences of slab rollback from c. 70 Ma and slab breakoff of the Neo-Tethyan oceanic lithosphere that began at c. 53 Ma. The India–Asia convergence was driven by Neo-Tethyan subduction with a normal rate of convergence at 120–95 Ma, ridge subduction at 95–85 Ma, then subduction of a young and buoyant oceanic lithosphere after ridge subduction with rate deceleration at 84–67 Ma, Deccan plume activity and slab rollback with rate acceleration at 67–51 Ma, slab breakoff for sudden drop of the convergence rate at c. 51 Ma, and finally the descent of the high-density Indian continental lithosphere beneath Asia since c. 50 Ma.