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all geography including DSDP/ODP Sites and Legs
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Admiralty Bay (1)
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Africa
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Congo Craton (2)
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East Africa
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Tanzania
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Olduvai Gorge (1)
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Limpopo Belt (3)
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Madagascar
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Mozambique Belt (1)
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Southern Africa
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Barberton greenstone belt (3)
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Botswana (1)
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Kaapvaal Craton (10)
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Namaqualand metamorphic complex (1)
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South Africa
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Bushveld Complex (1)
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Limpopo South Africa (1)
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Mpumalanga South Africa
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Barberton Mountain Land (1)
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Northern Cape Province South Africa (1)
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Transvaal region (1)
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Witwatersrand (6)
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West Africa
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Zimbabwe Craton (1)
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Antarctica
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Arctic region
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Asia
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Karnataka India
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Irkutsk Russian Federation (2)
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Middle East
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Turkey
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Okhotsk-Chukchi volcanic belt (1)
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Atlantic Ocean
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Australasia
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Australia
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New Zealand
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Eastern Canada
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Ontario
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Quebec (1)
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Western Canada
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Manitoba (1)
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Caribbean region
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Antilles
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Haiti
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Lesser Antilles
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Central America
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Chukotka Russian Federation (1)
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Europe
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Central Europe
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United Kingdom
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Scotland
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Wales
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Hikurangi Margin (1)
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Indian Ocean
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East Indian Ocean (1)
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Indian Ocean Islands
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Madagascar
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Mahajanga Basin (1)
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Jack Hills (1)
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Mascarene Basin (1)
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Mexico (1)
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North America
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Canadian Shield
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Superior Province
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Abitibi Belt (1)
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Gulf Coastal Plain (1)
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Rocky Mountains
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U. S. Rocky Mountains
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Absaroka Range
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Shuswap Complex (1)
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North Island (17)
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Oceania
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Melanesia
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Fiji
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Viti Levu (1)
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Pacific Ocean
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South Pacific
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Southwest Pacific
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Cook Strait (1)
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Hikurangi Trough (4)
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West Pacific
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Southwest Pacific
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Cook Strait (1)
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Hikurangi Trough (4)
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Price River basin (1)
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Scotia Sea Islands
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South Shetland Islands
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King George Island (1)
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South America
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Brazil
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Brasilia Belt (1)
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South Island (5)
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Thames River (1)
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United States
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Texas
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U. S. Rocky Mountains
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Utah
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Emery County Utah (1)
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commodities
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diamond deposits (1)
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gold ores (11)
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lead ores (1)
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lead-zinc deposits (1)
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nickel ores (1)
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mineral deposits, genesis (11)
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mineral exploration (7)
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placers (2)
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elements, isotopes
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carbon
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C-14 (3)
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chemical elements (1)
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chemical ratios (1)
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halogens
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chlorine
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chloride ion (1)
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fluorine (2)
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hydrogen (1)
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isotope ratios (17)
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isotopes
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radioactive isotopes
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C-14 (3)
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U-238/U-235 (1)
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stable isotopes
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C-13/C-12 (2)
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Hf-177/Hf-176 (6)
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Nd-144/Nd-143 (2)
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O-18/O-16 (6)
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Pb-207/Pb-206 (1)
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Sr-87/Sr-86 (4)
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Lu/Hf (3)
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metals
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actinides
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thorium (3)
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uranium
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U-238/U-235 (1)
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alkali metals
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lithium (1)
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potassium (1)
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alkaline earth metals
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beryllium (7)
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magnesium (1)
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strontium
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Sr-87/Sr-86 (4)
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aluminum (2)
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antimony (2)
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arsenic (1)
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gold (1)
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hafnium
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Hf-177/Hf-176 (6)
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iron
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ferrous iron (1)
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lead
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Pb-207/Pb-206 (1)
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manganese (2)
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niobium (3)
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platinum group
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iridium (1)
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precious metals (1)
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rare earths
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cerium (1)
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europium (1)
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neodymium
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Nd-144/Nd-143 (2)
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samarium (1)
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yttrium (2)
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titanium (2)
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zinc (2)
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oxygen
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O-18/O-16 (6)
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phosphorus (1)
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fossils
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Invertebrata
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Insecta
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Pterygota
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Diptera
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Chironomidae (1)
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Echinodermata
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problematic fossils
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thermochronology (1)
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U/Pb (32)
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U/Th/Pb (3)
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geologic age
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Cenozoic
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Quaternary
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Holocene (5)
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Pleistocene
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upper Pleistocene
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upper Weichselian
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Allerod (2)
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Wisconsinan
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upper Wisconsinan (1)
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Tertiary
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Neogene
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Paleogene
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upper Oligocene (1)
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Paleocene
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lower Paleocene
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upper Cenozoic (1)
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Cretaceous
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Jurassic (2)
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Paleozoic
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Devonian
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Upper Devonian
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lower Paleozoic (4)
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Ordovician
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Lower Ordovician
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Permian (2)
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upper Paleozoic (1)
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Precambrian
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Paleoarchean (2)
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Central Rand Group (3)
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upper Precambrian
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Mesoproterozoic (2)
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Neoproterozoic (11)
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Paleoproterozoic
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Rooiberg Group (1)
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Ventersdorp Supergroup (1)
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Waterberg System (1)
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igneous rocks
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igneous rocks
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two-mica granite (1)
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porphyry (2)
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pyroclastics
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metamorphic rocks
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metamorphic rocks
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granulites (17)
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marbles
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metacarbonate rocks (2)
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metaigneous rocks
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metabasite (2)
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metasedimentary rocks
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metapelite (6)
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metasomatic rocks
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native elements
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orthopyroxene
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framework silicates
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feldspar group
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alkali feldspar
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K-feldspar (4)
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silica minerals
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opal (1)
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quartz (4)
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orthosilicates
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dumortierite (1)
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garnet group
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majorite (1)
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kyanite (3)
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olivine group
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fayalite (1)
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forsterite (1)
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ringwoodite (1)
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sillimanite (4)
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staurolite (1)
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titanite group
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titanite (2)
-
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Journal Article
The New Zealand earthquake of February 3, 1931
Publisher: Seismological Society of America
Published: 01 December 1931
Bulletin of the Seismological Society of America (1931) 21 (4): 251–260.
..., the Napier Boys' High School, a brick structure, stands nobly save for insignificant damage, if we except the Assembly Hall, the inadequate foundation of which accounts for 1 See Figure 2, Plate 26. 254 BULLETIN OF TtIE SEISMOLOGICAL SOCIETY OF AMERICA its destr.uction. The conclusion to which one is forced...
Journal Article
Modeling and Estimating Post-Earthquake Fire Spread
Journal: Earthquake Spectra
Publisher: Earthquake Engineering Research Institute
Published: 01 May 2012
Earthquake Spectra (2012) 28 (2): 795–810.
.... In the model, it is assumed that all roofs other than concrete roofs are not fire-rated and that fire spread via roofs will only occur if the adjacent building is within two cells distance (6 m), based on the separation distance stated in the New Zealand Building Code Handbook (DBH 2008). The Napier...
Journal Article
Further notes on certain horizontal pendulum movements
Publisher: Seismological Society of America
Published: 01 July 1940
Bulletin of the Seismological Society of America (1940) 30 (3): 219–224.
...F. Napier Denison Copyright © 1940, by the Seismological Society of America * Manuscript received for publication August 5, 1939. FURTHER NOTES ON CERTAIN HORIZONTAL PENDULUM MOVEMENTS* By F. NAPmRDE ISO AT THE CLOSEof 1938, thirty-six years of daily observations from the E - W...
Journal Article
Hazard Sensitivities Associated with Ground‐Motion Characterization Modeling for the New Zealand National Seismic Hazard Model Revision 2022
Sanjay S. Bora, Brendon A. Bradley, Elena F. Manea, Matthew C. Gerstenberger, Robin L. Lee, Peter J. Stafford, Gail M. Atkinson, Anna Kaiser, Christopher J. DiCaprio, Russell J. Van Dissen
Publisher: Seismological Society of America
Published: 06 December 2023
Bulletin of the Seismological Society of America (2024) 114 (1): 422–448.
... 5 . The same plots for Hamilton, Napier, New Plymouth, and Dunedin are shown in the supplemental material. From these plots, it is clear that the SI sources dominate hazard along the eastern coast of North Island (Wellington, Napier) and in the southwestern part of the South Island (Te Anau). In low...
Includes: Supplemental Content
Journal Article
A 5000 yr record of coastal uplift and subsidence reveals multiple source faults for past earthquakes on the central Hikurangi margin, New Zealand
Charlotte Pizer, Kate Clark, Jamie Howarth, Andrew Howell, Jaime Delano, Bruce W. Hayward, Nicola Litchfield
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 15 November 2023
GSA Bulletin (2024) 136 (7-8): 2702–2722.
... faulting prevent reliable indication of source faults. In this work, we improved paleoearthquake reconstructions on the central Hikurangi margin with a new, well-constrained 5000 yr earthquake record from Pakuratahi Valley near Napier, North Island, New Zealand. Evidence of laterally extensive...
Journal Article
Chevkinite-group minerals from granulite-facies metamorphic rocks and associated pegmatites of East Antarctica and South India
Journal: Mineralogical Magazine
Published: 01 February 2009
Mineralogical Magazine (2009) 73 (1): 149–164.
...H. E. Belkin; R. Macdonald; E. S. Grew Abstract Electron microprobe data are presented for chevkinite-group minerals from granulite-facies rocks and associated pegmatites of the Napier Complex and Mawson Station charnockite in East Antarctica and from the Eastern Ghats, South India...
Journal Article
Development and Calibration of an Earthquake Fatality Function
Journal: Earthquake Spectra
Publisher: Earthquake Engineering Research Institute
Published: 01 August 2003
Earthquake Spectra (2003) 19 (3): 605–633.
... of urban areas where this method is directly applicable. The events selected for study were the 1886 Charleston, South Carolina; 1915 Avez- zano, Italy; 1931 Napier, New Zealand; and 1976 Tangshan, China, earthquakes. Each of these earthquakes had death tolls in excess of one percent of the population...
Journal Article
Estimating Slab Earthquake Response Spectra from a 3D Q Model
Publisher: Seismological Society of America
Published: 01 December 2003
Bulletin of the Seismological Society of America (2003) 93 (6): 2649–2663.
...-loss slab paths, such as Napier, than at closer sites with paths through the mantle wedge. Deep earthquakes have produced triggered strong-motion records at eastern sites, but for engineering applications the response for deep earthquakes at sites including high-loss paths, such as Taupo and Rotorua...
Journal Article
Crustal structure and properties of Archean cratons of Gondwanaland: similarity and difference
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2018
Russ. Geol. Geophys. (2018) 59 (5): 512–524.
... age and lithology, Moho depth, thickness of lithosphere and sediments, as well as elevations, all summarized in a table. The cratons differ in size from 0.05 × 10 6 km 2 (Napier craton) to 4 × 10 6 km 2 (Congo craton) and span almost the entire Archean period from 3.8 to 2.5 Ga. Sediments are mostly...
Journal Article
Synthesis of beryllian sapphirine in the system MgO-BeO-Al 2 O 3 -SiO 2 -H 2 O and comparison with naturally occurring beryllian sapphirine and khmaralite, Part 2: A chemographic study of Be content as a function of P , T, assemblage and FeMg –1 exchange
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 February 2004
American Mineralogist (2004) 89 (2-3): 327–338.
.... At higher T, maximum Be increases with P, following the MBeAS univariant reactions involving (sapphirine + surinamite + orthopyroxene + chrysoberyl + forsterite or spinel). Natural assemblages containing sapphirine and its Be-rich near-analog khmaralite from the Napier Complex, Enderby Land, East Antarctica...
Journal Article
Tibetan Plateau insights into >1100 °C crustal melting in the Quaternary
Journal: Geology
Publisher: Geological Society of America
Published: 20 October 2022
Geology (2022) 50 (12): 1432–1437.
..., and an anonymous reviewer for constructive suggestions. This study was jointly supported by the National Natural Science Foundation of China (grants 91855215, 41872065, and 42021002), and the Second Tibetan Plateau Scientific Expedition and Research program (STEP) (grant 2019QZKK0702). This is contribution IS-3235...