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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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West Africa
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Sierra Leone (1)
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Arctic Ocean
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Norwegian Sea (1)
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Asia
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Far East
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Japan (2)
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Atlantic Ocean
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North Atlantic
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Blake-Bahama Outer Ridge (1)
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Canada
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Western Canada
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British Columbia (1)
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Caribbean region
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West Indies
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Antilles
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Caspian Sea (1)
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Central America
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Chortis Block (1)
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Costa Rica
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Guatemala (1)
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Panama
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Europe
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Pacific Ocean
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South Pacific
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fossils
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Nicoya Complex (4)
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igneous rocks
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Primary terms
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absolute age (4)
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Africa
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West Africa
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Sierra Leone (1)
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Arctic Ocean
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Norwegian Sea (1)
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Asia
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Far East
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Japan (2)
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-
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Atlantic Ocean
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North Atlantic
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Blake-Bahama Outer Ridge (1)
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Canada
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Western Canada
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British Columbia (1)
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-
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carbon
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C-14 (2)
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organic carbon (1)
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Caribbean region
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West Indies
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Antilles
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Lesser Antilles
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Barbados (1)
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Caspian Sea (1)
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Cenozoic
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Quaternary
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upper Quaternary (1)
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Tertiary
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lower Tertiary (1)
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Paleogene
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Eocene
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lower Eocene (1)
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Paleocene
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lower Paleocene
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K-T boundary (1)
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Central America
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Chortis Block (1)
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Costa Rica
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Nicoya Peninsula (19)
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Guatemala (1)
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Nicaragua (4)
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Panama
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Darien (1)
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clay mineralogy (2)
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continental shelf (1)
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crust (10)
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crystal chemistry (1)
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data processing (2)
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Deep Sea Drilling Project
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IPOD
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Leg 56
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DSDP Site 434 (1)
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Leg 84
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DSDP Site 570 (1)
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deformation (2)
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diagenesis (1)
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earthquakes (8)
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education (1)
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Europe
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Alps
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Central Europe
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geochemistry (7)
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heat flow (2)
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hydrology (1)
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igneous rocks
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granophyre (1)
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kimberlite (1)
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plutonic rocks
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diabase (1)
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volcanic rocks
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basalts
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mid-ocean ridge basalts (1)
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glasses
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volcanic glass (1)
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rhyolites (1)
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Integrated Ocean Drilling Program (1)
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intrusions (1)
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Invertebrata
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Protista
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Foraminifera (2)
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Radiolaria (1)
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isotopes
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radioactive isotopes
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Be-10 (1)
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C-14 (2)
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stable isotopes
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Li-6 (1)
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Li-7 (1)
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lava (1)
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magmas (2)
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mantle (1)
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maps (1)
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Mediterranean Sea
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East Mediterranean (1)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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K-T boundary (1)
-
-
-
Nicoya Complex (4)
-
-
metals
-
alkali metals
-
lithium
-
Li-6 (1)
-
Li-7 (1)
-
-
-
alkaline earth metals
-
beryllium
-
Be-10 (1)
-
-
calcium (1)
-
-
iron
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ferric iron (1)
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-
-
metamorphic rocks
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eclogite (1)
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metamorphism (1)
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metasomatism (2)
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meteorites
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stony meteorites
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chondrites (1)
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Mohorovicic discontinuity (1)
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mud volcanoes (3)
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North America
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Basin and Range Province
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Great Basin (1)
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-
-
Ocean Drilling Program
-
Leg 110 (1)
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Leg 112
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ODP Site 685 (1)
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-
Leg 131 (2)
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Leg 146
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ODP Site 889 (1)
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Leg 160 (1)
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Leg 164
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ODP Site 994 (1)
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ODP Site 995 (1)
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ODP Site 997 (1)
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-
Leg 170
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ODP Site 1039 (5)
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ODP Site 1040 (6)
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ODP Site 1041 (1)
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ODP Site 1043 (4)
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Leg 190 (1)
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Leg 205
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ODP Site 1253 (1)
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ODP Site 1254 (1)
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ODP Site 1255 (1)
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-
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ocean floors (10)
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orogeny (1)
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Pacific Ocean
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East Pacific
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Cocos Ridge (1)
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Galapagos Rift (1)
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Northeast Pacific
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Gulf of Panama (1)
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Middle America Trench (11)
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Southeast Pacific (2)
-
-
Equatorial Pacific (2)
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North Pacific
-
Northeast Pacific
-
Gulf of Panama (1)
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Middle America Trench (11)
-
-
Northwest Pacific
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Japan Trench (1)
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Nankai Trough (1)
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Okhotsk Sea (1)
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-
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South Pacific
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Southeast Pacific (2)
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West Pacific
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Northwest Pacific
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Japan Trench (1)
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Nankai Trough (1)
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Okhotsk Sea (1)
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paleogeography (1)
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paleomagnetism (1)
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petroleum (1)
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plate tectonics (20)
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sedimentary petrology (1)
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sedimentary rocks
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carbonate rocks
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chalk (1)
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clastic rocks
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sandstone (1)
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sedimentation (2)
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sediments
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clastic sediments
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mud (1)
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marine sediments (9)
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shorelines (1)
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soils
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South America
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Chile (1)
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spectroscopy (1)
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tectonics
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neotectonics (3)
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United States
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Great Basin (1)
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weathering (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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beachrock (1)
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chalk (1)
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clastic rocks
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sandstone (1)
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volcaniclastics (1)
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sedimentary structures
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sediments
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sediments
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clastic sediments
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mud (1)
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marine sediments (9)
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volcaniclastics (1)
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soils
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paleosols (1)
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soils
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laterites (1)
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GeoRef Categories
Era and Period
Epoch and Age
Date
Availability
Collision of the Caribbean Large Igneous Province with the Americas: Earliest evidence from the forearc of Costa Rica
Scaly fabric and slip within fault zones
Hydrothermal circulation and the thermal structure of shallow subduction zones
KAOLINITE AND HALLOYSITE DERIVED FROM SEQUENTIAL TRANSFORMATION OF PEDOGENIC SMECTITE AND KAOLINITE-SMECTITE IN A 120 ka TROPICAL SOIL CHRONOSEQUENCE
Do subducting seamounts generate or stop large earthquakes?
Integration of Arrival‐Time Datasets for Consistent Quality Control: A Case Study of Amphibious Experiments along the Middle America Trench
The thickness of subduction plate boundary faults from the seafloor into the seismogenic zone
Experimental evidence linking slip instability with seafloor lithology and topography at the Costa Rica convergent margin
Do subducting seamounts generate or stop large earthquakes?
International field experiences offer exceptional opportunities for effective student learning in the geosciences. Over the 10 yr period between 1998 and 2008, more than 40 undergraduate students from 14 institutions participated in field research investigating active tectonics on the Nicoya Peninsula, Costa Rica. Three different project models were used: (1) a month-long summer research project, (2) a series of 1 to 2 wk independent field study projects, and (3) a week-long field research module. These projects shared a common research theme (active tectonics), field area (Nicoya Peninsula), and pedagogy (experiential learning), thus allowing for easy comparison of teaching methods, logistics, and learning outcomes. Each model has unique pedagogical benefits and challenges, and is therefore better suited for a different group size, student to faculty ratio, project duration, and budget. Collectively, these student research projects generated significant publishable data relevant to ongoing investigations of forearc tectonics and earthquake hazards along the Costa Rican Pacific margin. Individual student projects were carefully designed to provide a quality field learning experience, while adding a new piece to the larger research puzzle. Indicators of project success include levels of student engagement; gains in technical and cognitive field skills; and productivity of student-authored publications, reports, and presentations. Students commonly described these projects as instrumental in shaping their professional identity as geoscientists. Blending international field research with experiential learning pedagogy creates a powerful synergy that captures student imagination and motivates learning. By placing students beyond the comfort of their home learning environment, international field projects pique student curiosity, sharpen awareness and comprehension, and amplify the desire to learn. Experiential learning pedagogy encourages students to define their own research agenda and solve problems through critical thinking, inquiry, and reflection. The potent combination of international fieldwork and experiential learning helps students to develop the self-confidence and reasoning skills needed to solve multifaceted real-world problems, and provides exceptional training for graduate school and professional careers in the geosciences.