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NARROW
Format
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GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Congo Democratic Republic (1)
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East African Rift (1)
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Southern Africa
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South Africa (1)
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Arctic region
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Svalbard
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Asia
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Arabian Peninsula
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Central Asia
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Pamirs (1)
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Far East
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Borneo
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Burma (5)
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China
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Malaysia
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East Malaysia
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Sabah Malaysia (1)
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West Malaysia
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Kedah Malaysia (1)
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Mongolia (3)
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Atlantic Ocean
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Commonwealth of Independent States
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Europe
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Southern Europe
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Transcaucasia (1)
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Indian Ocean
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Bay of Bengal
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Kutei Basin (1)
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Malay Archipelago
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Borneo
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Pacific Ocean
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West Pacific
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South America
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chemical ratios (2)
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hydrogen
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isotope ratios (6)
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Hf-177/Hf-176 (1)
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O-18/O-16 (3)
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large-ion lithophile elements (1)
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iron (3)
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vanadium (1)
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zirconium (1)
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nitrogen
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N-15/N-14 (1)
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noble gases
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radon
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Rn-222 (1)
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-
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oxygen
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O-18/O-16 (3)
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phosphorus (1)
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fossils
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Chordata
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Vertebrata
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Pisces (1)
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Tetrapoda
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Mammalia
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Theria
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Eutheria
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Carnivora
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Fissipeda
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Reptilia
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Diapsida
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Archosauria
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dinosaurs
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Graptolithina
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Hemichordata (2)
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Invertebrata
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Arthropoda
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Brachiopoda
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Articulata
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Porites (1)
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Mollusca
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Cephalopoda
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Goniatitida
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Goniatitidae
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Nautiloidea (1)
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Protista
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Foraminifera
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microfossils
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Conodonta (4)
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Pterobranchia (2)
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geochronology methods
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paleomagnetism (1)
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Rb/Sr (2)
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U/Pb (5)
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geologic age
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Cenozoic
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Quaternary
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Tertiary
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Neogene
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Pliocene (3)
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Paleogene
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Oligocene (2)
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-
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Mesozoic
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Cretaceous
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Comanchean
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Travis Peak Formation (1)
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Lower Cretaceous
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Travis Peak Formation (1)
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Upper Cretaceous (1)
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Jurassic (1)
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Triassic
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Lower Triassic
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Permian-Triassic boundary (1)
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Middle Triassic (1)
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Upper Triassic
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Carnian (1)
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Norian (1)
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Paleozoic
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Cambrian
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Upper Cambrian
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Furongian (2)
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Carboniferous
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Namurian (1)
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Upper Carboniferous (1)
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Devonian
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Lower Devonian (2)
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Upper Devonian (1)
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lower Paleozoic (1)
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middle Paleozoic (1)
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Ordovician
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Lower Ordovician
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Ibexian (1)
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Upper Ordovician
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Hirnantian (1)
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-
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Permian
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Guadalupian (1)
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Lower Permian
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Cisuralian
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Kungurian (1)
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-
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Upper Permian
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Lopingian
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Changhsingian (1)
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Permian-Triassic boundary (1)
-
-
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Phuket Group (5)
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Silurian
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Lower Silurian
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Llandovery
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Rhuddanian (1)
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-
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Phanerozoic (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Neoproterozoic (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites
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aplite (2)
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biotite granite (2)
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I-type granites (3)
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S-type granites (3)
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pegmatite (3)
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ultramafics
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peridotites
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spinel lherzolite (1)
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volcanic rocks
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basalts
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alkali basalts (3)
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pyroclastics
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ignimbrite (1)
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rhyolites (1)
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metamorphic rocks
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metamorphic rocks
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gneisses
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metasedimentary rocks (1)
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metasomatic rocks
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minerals
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rutile (2)
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orthosilicates
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zircon group
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zircon (10)
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ring silicates
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sheet silicates
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chlorite group
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clay minerals
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illite (2)
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mica group
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sulfides
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pyrite (2)
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tungstates
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wolframite (2)
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Primary terms
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absolute age (8)
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Africa
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Central Africa
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Congo Democratic Republic (1)
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East African Rift (1)
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Southern Africa
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South Africa (1)
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Arctic region
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Svalbard
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Asia
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Arabian Peninsula
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Oman (1)
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Central Asia
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Pamirs (1)
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Far East
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Borneo
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East Malaysia
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Sarawak Malaysia (1)
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Burma (5)
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China
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Inner Mongolia China (2)
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Yangtze Platform (1)
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Indochina (4)
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Indonesia
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Japan (6)
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Korea (2)
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Laos (3)
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Lesser Sunda Islands
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Malay Peninsula
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Kedah Malaysia (1)
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Kelantan Malaysia (2)
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Langkawi Islands (7)
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Pahang Malaysia (1)
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Selangor Malaysia
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Kuala Lumpur Malaysia (1)
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-
-
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Malaysia
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East Malaysia
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Sabah Malaysia (1)
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Sarawak Malaysia (1)
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-
West Malaysia
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Kedah Malaysia (1)
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Kelantan Malaysia (2)
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Langkawi Islands (7)
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Pahang Malaysia (1)
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Selangor Malaysia
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Kuala Lumpur Malaysia (1)
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Mongolia (3)
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Philippine Islands (4)
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Taiwan (2)
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Thailand
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Bangkok Thailand (1)
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Chiang Mai Thailand (1)
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Khorat Plateau (1)
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Vietnam (4)
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Himalayas (1)
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Indian Peninsula
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Afghanistan (1)
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Bangladesh (1)
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India (4)
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Pakistan
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Punjab Pakistan
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Salt Range (1)
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-
-
-
Karakoram (1)
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Mekong River (1)
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Middle East
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Iran (1)
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Turkey (1)
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Okhotsk region (1)
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Primorye Russian Federation (1)
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Qiangtang Terrane (1)
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Southeast Asia (7)
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Sri Lanka (1)
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Verkhoyansk region (1)
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associations (1)
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Atlantic Ocean
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North Atlantic
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Gulf of Mexico (1)
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-
-
Australasia
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Australia
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Queensland Australia (1)
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Western Australia (2)
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-
New Zealand (1)
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biogeography (6)
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biography (1)
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boron (1)
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Canada
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Western Canada (1)
-
-
carbon
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C-13/C-12 (2)
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organic carbon (1)
-
-
Caribbean region
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West Indies
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Bahamas (1)
-
-
-
Cenozoic
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Quaternary
-
Holocene (4)
-
Pleistocene
-
upper Pleistocene (1)
-
-
-
Tertiary
-
Neogene
-
Miocene
-
middle Miocene (1)
-
upper Miocene (1)
-
-
Pliocene (3)
-
-
Paleogene
-
Eocene (4)
-
Oligocene (2)
-
-
-
-
Chordata
-
Vertebrata
-
Pisces (1)
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Carnivora
-
Fissipeda
-
Mustelidae (1)
-
-
-
-
-
-
Reptilia
-
Diapsida
-
Archosauria
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dinosaurs
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Ornithischia (1)
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-
-
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clay mineralogy (6)
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continental drift (2)
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earthquakes (3)
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Europe
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Iberian Peninsula
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Transcaucasia (1)
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geochronology (2)
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geophysical methods (35)
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hydrogen
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D/H (1)
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igneous rocks
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plutonic rocks
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granites
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aplite (2)
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biotite granite (2)
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I-type granites (3)
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S-type granites (3)
-
-
pegmatite (3)
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ultramafics
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peridotites
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spinel lherzolite (1)
-
-
-
-
volcanic rocks
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basalts
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alkali basalts (3)
-
-
pyroclastics
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ignimbrite (1)
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rhyolites (1)
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inclusions
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fluid inclusions (1)
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Indian Ocean
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Bay of Bengal
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Andaman Basin (1)
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intrusions (3)
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Invertebrata
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Arthropoda
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Trilobitomorpha
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Trilobita
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Corynexochida (1)
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Phacopida
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Phacopina (1)
-
-
-
-
-
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Anisotropy estimation from deviated wells: uncertainties and their implications — A case study Available to Purchase
A HISTORY OF 20 TH CENTURY GRAPTOLITE STUDIES IN MALAYSIA: THE ROLE OF CLIVE RODERICK JONES Available to Purchase
A New Crustal Thickness and V P / V S Model of the Indochina Peninsula Available to Purchase
SE Asia as part of Gondwana: a 1960s regional mapping project over Southern Thailand that lay behind the hypothesis Available to Purchase
Abstract In the 1960s, anticipating the award of concessions in the Gulf of Thailand, BP carried out reconnaissance geological mapping over all of Southern Thailand including its Gulf islands. The resulting eight geological maps at 1:250 000 scale provided a database that underpinned discussions of Thailand's place in global plate-tectonic reconstructions that were emerging at that time. In particular, new light was thrown on the Paleozoic succession, and important differences were found between the Upper Thai Peninsula and the Lower Peninsula (respectively, NW and SE of the prominent bend in the peninsula's outline). The Phuket Group of the Upper Peninsula is a very thick diamictite-bearing succession of possible Devonian to Early Permian age, apparently sourced in the west, a region now occupied by the Indian Ocean. That in turn suggested a possible Gondwana origin for SE Asia, a contentious concept at the time, but one that is now widely accepted. The emphasis of field mapping these days is on obtaining detailed data that necessarily means over areas of limited extent. But a very broad regional mapping project such as BP's in Thailand revealed stratigraphic and tectonic insights that could be revealed only from a wide-ranging regional study of this kind.
The Late Cambrian to Neogene Evolution of the Khanom Core Complex (Peninsular Thailand) Open Access
Detrital zircon U–Pb and Hf analyses of Silurian–Devonian sediments in the Sukhothai Terrane, northern Thailand: implications for the Mid-Paleozoic arc belt Available to Purchase
A decade of successful magnetotelluric surveys for delineating shallow geothermal reservoirs beneath nonvolcanic hot springs in Thailand Available to Purchase
Latest Ordovician to earliest Silurian graptolites of northwest Peninsular Malaysia Available to Purchase
Plume-related, syn-rift, Neogene volcanism, the interplay with structure in Thailand and comparison with the East African Rift Available to Purchase
The Effect of Size Distribution on the Geochemistry and Mineralogy of Tropical River Sediments and Its Implications regarding Chemical Weathering and Fractionation of Alkali Elements Open Access
Distribution of 222 Rn in Seawater Intrusion Area and Its Implications on Tracing Submarine Groundwater Discharge on the Upper Gulf of Thailand Open Access
Characterizing the subsea Pleistocene fluvial system of the Sunda shelf, offshore Malaysia, using multiattribute corendering and self-organizing maps Available to Purchase
Historical and emerging super basins of Southeast Asia Available to Purchase
Thailandina and Neothailandina and their family Thailandinidae salvaged: a valid taxonomic group of peculiar Permian fusuline Foraminifera Open Access
Late Permian ultrapotassic rhyolites in SE Thailand: evidence for a Palaeotethyan continental rift basin Available to Purchase
Satunarcus , a new late Cambrian trilobite genus from southernmost Thailand and a reevaluation of the subfamily Mansuyiinae Hupé, 1955 Available to Purchase
Reducing seismic reflector distortion beneath gas clouds in the Malay Basin using full-wavefield imaging approaches Available to Purchase
Validation and analysis procedures for juxtaposition and membrane fault seals in oil and gas exploration Open Access
Abstract We propose and validate methods for risk analysis of fault-bounded hydrocarbon traps in exploration. We concentrate on cross-fault leakage and consider lateral seals due to (1) juxtaposition and (2) high capillary-entry-pressure fault rock (membrane seal). We conclude that stochastic methods for fault seal analysis are essential, due to the large number of structural and stratigraphic parameters and the uncertainties. Central to the methods proposed is a Monte Carlo simulation which models geometrical and stratigraphic uncertainty. Multiple Allan maps (fault-parallel cross-sections) are produced and analysed for juxtaposition and shale gouge ratio (SGR). For validation, known discoveries with independently observed hydrocarbon–water contacts (IHWC) have been back-analysed. We present two case studies in this paper, and an additional 40 case studies are summarized (four public domain and 36 confidential case studies). The model outputs were compared with the IHWC. Juxtaposition analysis with no SGR contribution gives the smallest error. The inclusion of any fault rock seal mechanisms (such as SGR) matches or increases predicted hydrocarbon column heights compared to juxtaposition and gives larger errors. We conclude there is no reason to include fault rock membrane seals in exploration prospect risking.