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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Kenya (2)
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Uganda (1)
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East African Rift (1)
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North Africa
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Egypt (2)
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Morocco
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Rif (1)
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Southern Africa
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Barberton greenstone belt (1)
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Kaapvaal Craton (2)
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Karoo Basin (1)
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Orange River (1)
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South Africa
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Northern Cape Province South Africa (1)
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Altiplano (10)
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Antarctica
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East Antarctica (1)
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Arctic Ocean
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Asia
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Far East
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Mexico
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Pacific Ocean
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North Pacific
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Japan Sea
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South Pacific
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Southeast Pacific
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Southwest Pacific
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West Pacific
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Mariana Trough (1)
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Puna (8)
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West Virginia
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Western U.S. (5)
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West Pacific Ocean Islands
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commodities
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elements, isotopes
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carbon
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chemical ratios (1)
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halogens
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chlorine
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Cl-36 (1)
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hydrogen
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deuterium (2)
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isotope ratios (14)
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isotopes
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radioactive isotopes
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Al-26 (3)
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (3)
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Pb-208/Pb-204 (3)
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stable isotopes
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C-13/C-12 (3)
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deuterium (2)
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He-3 (1)
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Nd-144/Nd-143 (4)
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O-18/O-16 (7)
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Pb-206/Pb-204 (3)
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Sr-87/Sr-86 (6)
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metals
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alkali metals
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potassium (1)
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alkaline earth metals
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beryllium
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Be-10 (5)
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strontium
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Sr-87/Sr-86 (6)
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aluminum
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Al-26 (3)
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lead
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (3)
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Pb-208/Pb-204 (3)
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mercury (1)
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platinum group
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rare earths
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neodymium
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Nd-144/Nd-143 (4)
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ytterbium (1)
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noble gases
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helium
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He-3 (1)
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oxygen
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O-18/O-16 (7)
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-
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fossils
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Vertebrata
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Mammalia (1)
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Invertebrata
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Cnidaria
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Mollusca
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Protista
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Foraminifera
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Rotaliina
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Cassidulinacea
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Cibicidoides (1)
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Globigerinacea
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Neogloboquadrina
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Neogloboquadrina pachyderma (1)
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Rotaliacea
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Nummulitidae
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Nummulites (1)
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Radiolaria (1)
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microfossils
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Conodonta (1)
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palynomorphs
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miospores
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Plantae
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algae
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nannofossils (3)
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Spermatophyta
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Nothofagus (1)
-
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thallophytes (2)
-
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geochronology methods
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Ar/Ar (15)
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exposure age (3)
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fission-track dating (10)
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geologic age
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Cenozoic
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Preboreal (1)
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Pleistocene
-
upper Pleistocene
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upper Quaternary (1)
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Sirius Group (1)
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Tertiary
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lower Tertiary (4)
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Neogene
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Miocene
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lower Miocene (3)
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middle Miocene (4)
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upper Miocene (5)
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Pliocene
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upper Neogene (1)
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Paleogene
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Eocene
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Oligocene
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upper Oligocene (1)
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-
Paleocene
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lower Paleocene
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K-T boundary (1)
-
-
-
-
-
upper Cenozoic (9)
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Laurentide ice sheet (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Middle Cretaceous (1)
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Upper Cretaceous
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Turonian (2)
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-
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Jurassic
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Triassic
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upper Mesozoic (2)
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MIS 5 (1)
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Paleozoic
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Cambrian (1)
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Carboniferous
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Namurian (1)
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Devonian
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Old Red Sandstone (2)
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Ordovician
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upper Paleozoic (1)
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Precambrian
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Archean
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Neoarchean (1)
-
-
upper Precambrian
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Proterozoic
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Mesoproterozoic (1)
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Neoproterozoic (2)
-
-
-
-
-
igneous rocks
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igneous rocks
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kimberlite (2)
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picrite (2)
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plutonic rocks
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alnoite (1)
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diorites
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tonalite (1)
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gabbros (3)
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granites
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granodiorites (1)
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lamprophyres
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minette (1)
-
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ultramafics
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peridotites
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lherzolite (1)
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spinel lherzolite (1)
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spinel peridotite (1)
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-
-
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volcanic rocks
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basalts
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alkali basalts (2)
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flood basalts (4)
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mid-ocean ridge basalts (1)
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tholeiite (1)
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tholeiitic basalt (1)
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basanite (1)
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dacites (1)
-
glasses
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volcanic glass (2)
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komatiite (2)
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melilitite (1)
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phonolites (1)
-
pyroclastics
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ash-flow tuff (1)
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ignimbrite (3)
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pumice (1)
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tuff (3)
-
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rhyolites (2)
-
-
-
wehrlite (1)
-
-
metamorphic rocks
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metamorphic rocks
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amphibolites (1)
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eclogite (2)
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gneisses
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biotite gneiss (2)
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orthogneiss (2)
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granulites (2)
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turbidite (1)
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minerals
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carbonates (1)
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hydrates (1)
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oxides
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phosphates
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apatite (17)
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monazite (3)
-
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silicates
-
chain silicates
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amphibole group
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clinoamphibole
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hornblende (1)
-
-
-
pyroxene group
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orthopyroxene (1)
-
-
-
framework silicates
-
feldspar group
-
alkali feldspar
-
sanidine (1)
-
-
-
zeolite group (1)
-
-
orthosilicates
-
nesosilicates
-
garnet group (1)
-
titanite group
-
titanite (1)
-
-
zircon group
-
zircon (11)
-
-
-
-
sheet silicates
-
mica group
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phlogopite (1)
-
-
-
-
wehrlite (1)
-
-
Primary terms
-
absolute age (39)
-
Africa
-
East Africa
-
Kenya (2)
-
Uganda (1)
-
-
East African Rift (1)
-
North Africa
-
Egypt (2)
-
Morocco
-
Rif (1)
-
-
-
Southern Africa
-
Barberton greenstone belt (1)
-
Kaapvaal Craton (2)
-
Karoo Basin (1)
-
Orange River (1)
-
South Africa
-
Northern Cape Province South Africa (1)
-
-
-
-
Antarctica
-
East Antarctica (1)
-
Transantarctic Mountains (1)
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West Antarctica (1)
-
-
Arctic Ocean
-
Eurasia Basin (1)
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Lomonosov Ridge (1)
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Mid-Arctic Ocean Ridge (1)
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Norwegian Sea (1)
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Yermak Plateau (3)
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Arctic region
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Greenland (2)
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Svalbard (1)
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Asia
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Amur region (1)
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Arabian Peninsula
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Oman (1)
-
-
Brahmaputra River (1)
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Central Asia
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Pamirs (1)
-
-
Far East
-
China
-
Gansu China
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plateaus
Localized Cenozoic erosion on the southern African Plateau: A signal of topographic uplift?
A Bayesian Lasso Logistic Regression Model for Predicting the Probability of Regional Seismic Phase Observation Using Sn in the Middle East and East Asia as Examples
Mesozoic denudation history of the lower Orange River and eastward migration of erosion across the southern African Plateau
Geochemical evidence for an orogenic plateau in the southern U.S. and northern Mexican Cordillera during the Laramide orogeny
Timing and mechanism of the rise of the Shillong Plateau in the Himalayan foreland
A lifetime of the Variscan orogenic plateau from uplift to collapse as recorded by the Prague Basin, Bohemian Massif
Editorial
Impact origin of Archean cratons
Genetic framework of Neogene–Quaternary basin closure process in central Turkey
Cenozoic Basin Evolution and Uplift History of the Central Andean Plateau, Southern Peru
Abstract In the central Andes of South America, a combination of crustal shortening and thickening, lithospheric densification and delamination, and surficial and climate interactions have resulted in development of the 3–5 km-high central Andean plateau and flanking 6–7 km peaks of the Eastern and Western cordilleras. Questions remain concerning the timing and rate of surface uplift and the relative roles of these mechanisms in producing and supporting these extreme elevations. End-member models attempting to answer these questions propose either a large-magnitude, rapid late Miocene uplift event, or rather slow and steady topographic growth initiating in the late Oligocene–early Miocene. The former model is based primarily on climate- and temperature-sensitive stable isotope analysis of carbonate material as a paleo-elevation proxy and is consistent with an uplift mechanism involving large-scale delamination and foundering of negatively buoyant lower crust and mantle lithosphere. The latter model is consistent with surface uplift driven directly by crustal shortening and is supported by climate simulations that suggest a nonlinear climate response to topographic uplift, indicating instead that there are threshold changes in temperature and isotopic composition of precipitation with rising topography, and highlighting that the use of such proxies may overestimate uplift rate and magnitude.