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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Egypt
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Sinai Egypt (1)
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Asia
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Far East
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Japan (1)
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Atlantic Ocean
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North Atlantic
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Caribbean Sea (1)
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Canada (1)
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Caribbean region
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West Indies
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Caribbean Mountain Range (1)
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Central America
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Costa Rica (1)
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Panama (1)
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Chama Basin (1)
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Llanos (3)
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North America
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Rocky Mountains
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U. S. Rocky Mountains
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Wind River Range (2)
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Pacific region (1)
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San Pedro Basin (1)
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Santander Massif (1)
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Andes
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Brazil
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Colombia
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Magdalena Delta (1)
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Magdalena Valley (1)
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Guajira Peninsula (8)
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Orinoco River (1)
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Peru (1)
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Venezuela
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Bocono Fault (2)
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Eastern Venezuela (1)
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Falcon Venezuela
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Paraguana Peninsula (1)
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Lake Maracaibo (31)
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Lara Venezuela (3)
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Maracaibo Basin (21)
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Maracaibo Falcon Plain (2)
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Merida Venezuela (6)
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Nueva Esparta Venezuela (1)
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Orinoco Delta (1)
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Tachira Venezuela (2)
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Trujillo Venezuela (1)
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Zulia Venezuela (4)
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Southern Ocean
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United States
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metals
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oxygen
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O-18/O-16 (2)
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fossils
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Chordata
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Vertebrata
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Osteichthyes
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Actinopterygii
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Teleostei
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Perciformes (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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Canidae
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Canis (1)
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Reptilia
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Anapsida
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Testudines
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Cyclostomata (1)
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ichnofossils (2)
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Invertebrata
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Porifera
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Protista
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Textulariina
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microfossils (13)
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palynomorphs
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Plantae
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algae
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oxides
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phosphates
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silicates
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orthosilicates
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sorosilicates
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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 (1)
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Primary terms
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Africa
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associations (1)
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Atlantic Ocean
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biogeography (5)
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Canada (1)
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carbon
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C-13/C-12 (5)
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Caribbean region
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Cenozoic
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Quaternary
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Holocene (3)
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Pleistocene
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upper Pleistocene
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upper Weichselian
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Younger Dryas (2)
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Tertiary
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Neogene
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upper Miocene (2)
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Pliocene (4)
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Paleogene
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Eocene
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lower Eocene
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Misoa Formation (6)
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middle Eocene
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Lutetian (1)
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Mirador Formation (2)
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upper Eocene (2)
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Oligocene
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lower Oligocene (1)
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upper Oligocene (1)
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Paleocene
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lower Paleocene
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Danian (1)
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K-T boundary (1)
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upper Paleocene (1)
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Pirabas Formation (1)
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Central America
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Panama (1)
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Chordata
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Vertebrata
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Pisces
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Osteichthyes
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Actinopterygii
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Teleostei
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Perciformes (1)
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Tetrapoda
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Mammalia
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Theria
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Eutheria
-
Carnivora
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Fissipeda
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Canidae
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Canis (1)
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Reptilia
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Anapsida
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Testudines
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intrusions (1)
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Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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-
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Bryozoa
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Scleractinia
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Mollusca
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
The Inachoididae spider crabs (Crustacea, Brachyura) from the Neogene of the tropical Americas Available to Purchase
Rapid screening and probabilistic estimation of the potential for CO 2 -EOR and associated geological CO 2 storage in Colombian petroleum basins Available to Purchase
Early Miocene coral reef-associated bryozoans from Colombia. Part I: Cyclostomata, “Anasca” and Cribrilinoidea Cheilostomata Open Access
Subsurface basement, structure, stratigraphy, and timing of regional tectonic events affecting the Guajira margin of northern Colombia Available to Purchase
Isotope sclerochronology indicates enhanced seasonal precipitation in northern South America (Colombia) during the Mid-Miocene Climatic Optimum Available to Purchase
Canopy structure in Late Cretaceous and Paleocene forests as reconstructed from carbon isotope analyses of fossil leaves Available to Purchase
Early Miocene shallow-water corals from La Guajira, Colombia: Part II, Mussidae–Siderastreidae and Milleporidae Available to Purchase
Early Miocene shallow-water corals from La Guajira, Colombia: part I, Acroporidae–Montastraeidae Available to Purchase
Perla Field: The Largest Discovery Ever in Latin America Available to Purchase
ABSTRACT Perla gas field is a world-class giant and one of the most significant in Latin America in the last decade. The field was discovered in August 2009. It is the largest gas field in Latin America with approximately 17 trillion cubic feet (tcf) of gas in place, or 3.1 BBOE. The field, located in the shallow waters of the Gulf of Venezuela, was discovered, and is operated by Cardon IV S.A., a 50/50 joint operating company formed by Repsol and Eni. The Perla discovery is important because it is a Play opener for the southern Caribbean domain, triggering a new exploration cycle in the region and proving a previously unknown Tertiary thermogenic petroleum system. The discovery well encountered a thick carbonate section (240 m [787 ft] thick) with excellent primary reservoir properties. The trap is a combination structural and stratigraphic, defined by a northwest–southeast trending asymmetric faulted structure and pinch-out of the carbonate reservoir rock to the north. The proven hydrocarbon column exceeds 350 m (1148 ft) and is in complete hydraulic continuity, and the structural-stratigraphic closure exceeds 100 km 2 (39 mi 2 ).
First record of buccinid genus Chauvetia (Mollusca: Gastropoda) from the fossil record of the New World (Miocene, Venezuela) and its paleobiogeographic implications Available to Purchase
New Evidence from a Black Mat Site in the Northern Andes Supporting a Cosmic Impact 12,800 Years Ago Available to Purchase
Strong tectonic and weak climatic control on exhumation rates in the Venezuelan Andes Open Access
New Bothremydid Turtle (Testudines, Pleurodira) from the Paleocene of Northeastern Colombia Available to Purchase
Association between magnetic susceptibilities and hydrocarbon deposits in the Barinas-Apure Basin, Venezuela Available to Purchase
A palynological zonation for the Cenozoic of the Llanos and Llanos Foothills of Colombia Available to Purchase
The new foraminiferal genus Ammogloborotaloides n. gen. and subfamily Ammogloborotaloidinae n. subfam. from the Neogene of Venezuela: an example of isomorphism between agglutinated and planktonic Foraminifera Available to Purchase
Asynchronous Miocene–Pliocene exhumation of the central Venezuelan Andes Available to Purchase
San Antonio de Mucuñó, Mérida Andes, Venezuela: Relocation of a doctrine town following the 1674 earthquake Available to Purchase
The prime cause of the relocation of one of the first villages founded in Venezuela by Spaniards in the early seventeenth century was likely motivated by earthquakes. San Antonio de Mucuñó, located in the Merida Andes ~200 km south-southeast of Maracaibo, was subjected to the effects of landslides triggered by a series of seismic events that took place in and around the year 1674. Historical documents, the geological and seismo-tectonic setting, and paleoseismic data support the conclusion that the earthquakes of 1674 occurred on the nearby, seismically active Bocono fault.