No. Registros Solicitud 1 5614 colombia



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RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

IS - ISSN: 0120-1425

CO - CODEN: #54470

AN - ACCESSION NUMBER: 2003-062814

UD - UPDATE CODE: 200320

Registro 327 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Cadena volcanica de Los Coconucos (Colombia), centros eruptivos y productos recientes

Translated Title: Los Coconucos volcanic belt (Colombia), volcanic centers and recent formations.

AU - AUTHORS: Monsalve-Maria-Luisa; Pulgarin-Bernardo

AF - AUTHOR AFFILIATION: Ingeominas, Unidad Operativa Popayan, Popayan, Colombia

SO - SOURCE: Boletin Geologico - Ingeominas. 37; 1-3, Pages 16-51. 1999.

PB - PUBLISHER: Instituto Nacional de Investigaciones Geologico-Mineras (INGEOMINAS). Bogota, Colombia. 1999.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1999

LA - LANGUAGE: Spanish

DE - DESCRIPTORS: andesites-; breccia-; calc-alkalic-composition; calderas-; Cauca-Colombia; chemical-composition; Colombia-; deformation-; eruptions-; explosive-eruptions; faults-; fumaroles-; geomorphology-; glaciers-; Huila-Colombia; hydrothermal-vents; igneous-rocks; landforms-; lava-flows; Los-Coconucos-volcanic-belt; major-elements; mineral-composition; minor-elements; Pan-de-Azucar; plate-tectonics; Purace-; pyroclastics-; soils-; South-America; stratigraphic-units; stratovolcanoes-; tectonostratigraphic-units; volcanic-ash; volcanic-breccia; volcanic-centers; volcanic-features; volcanic-rocks; volcanism-; volcanoes-

CC - CATEGORY CODES: 24-Quaternary-geology; 05A-Igneous-and-metamorphic-petrology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

MC - MAP COORDINATES: LAT: N021500; N022300; LONG: W0762000; W0762500.

IL - ILLUSTRATION: Refs: 33; illus. incl. strat. col., geol. sketch map.

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

IS - ISSN: 0120-1425

CO - CODEN: #54470

AN - ACCESSION NUMBER: 2003-062813

UD - UPDATE CODE: 200320

Registro 328 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Caldera de Paletara; aproximacion a la fuente de las ignimbritas del Cauca y Huila (Colombia)

Translated Title: Paletara Caldera, source of the Cauca and Huila (Colombia) ignimbrites?.

AU - AUTHORS: Torres-Maria-Patricia; Monsalve-Maria-Luisa; Pulgarin-Bernardo; Cepeda-Hector

AF - AUTHOR AFFILIATION: Ingeominas, Observatorio Vulcanologico y Sismologico, Popayan, Colombia

SO - SOURCE: Boletin Geologico - Ingeominas. 37; 1-3, Pages 1-15. 1999.

PB - PUBLISHER: Instituto Nacional de Investigaciones Geologico-Mineras (INGEOMINAS). Bogota, Colombia. 1999.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1999

LA - LANGUAGE: Spanish

DE - DESCRIPTORS: andesitic-composition; basins-; calderas-; Cauca-Colombia; Cenozoic-; Central-Cordillera; chemical-composition; Colombia-; deformation-; erosion-; faults-; geochemical-anomalies; geomorphology-; ground-water; helium-; hot-springs; Huila-Colombia; igneous-rocks; ignimbrite-; intrusions-; isotopes-; Landsat-; lava-flows; Magdalena-Valley; Mesozoic-; metamorphic-rocks; mineral-composition; noble-gases; Paleozoic-; Paletara-Caldera; Pan-de-Azucar; phreatomagmatism-; Pleistocene-; Purace-; pyroclastics-; Quaternary-; remote-sensing; rhyolitic-composition; satellite-methods; sedimentary-rocks; South-America; springs-; thermal-waters; volcanic-features; volcanic-rocks; volcanism-; volcanoes-

CC - CATEGORY CODES: 24-Quaternary-geology; 05A-Igneous-and-metamorphic-petrology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

MC - MAP COORDINATES: LAT: N020000; N023000; LONG: W0761000; W0764000.

IL - ILLUSTRATION: Refs: 22; illus. incl. geol. sketch map.

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

IS - ISSN: 0120-1425

CO - CODEN: #54470

AN - ACCESSION NUMBER: 2003-062812

UD - UPDATE CODE: 200320

Registro 329 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Holocene vegetation and climate variability in the Americas.

AU - AUTHORS: Grimm-Eric-C; Lozano-Garcia-Socorro; Behling-Hermann; Markgraf-Vera

AF - AUTHOR AFFILIATION: Illinois State Museum, Research and Collections Center, Springfield, IL, United States

BK - BOOK TITLE: In: Interhemispheric climate linkages.

BA - BOOK AUTHORS: Markgraf-Vera (editor)

SO - SOURCE: Pages 325-370. 2001.

PB - PUBLISHER: Academic Press. San Diego, CA, United States. 2001.

CP - COUNTRY OF PUBLICATION: United-States

PY - PUBLICATION YEAR: 2001

LA - LANGUAGE: English

LS - LANGUAGE OF SUMMARY: Spanish

AB - ABSTRACT: The striking feature of Holocene climate change along the Pole-Equator-Pole: Americas (PEP1) transect is that both hemispheres were generally warmer and drier in the early and middle Holocene than they are today, but with some exceptions. In North America, the northwestern and southeastern parts of the continent were warmer and drier because of increased insolation and strengthening of both the Bermuda High and the Eastern Pacific Subtropical High. However, the heat low in the midcontinent strengthened the monsoon in the southwestern United States, which was wetter in the early to middle Holocene than it is today, although still warmer. In the southwestern United States and the basin of Mexico, seasonality of precipitation was enhanced in the early Holocene with different results in the mountains and lowlands. Wetter conditions also existed in a band from Texas to the eastern Midwest. Northeast Canada, which was still covered by the Laurentide ice sheet, was the exception to an early Holocene thermal maximum. In South America, the early Holocene was also warmer and drier in most areas both north and south of the equator. In the lowlands, savanna regions were drier over a larger area than they are today, and the Andes were drier from Colombia to Tierra del Fuego, except at high elevations in northern Argentina and Chile. During the early and middle Holocene, westerly storm tracks were more tightly focused than they are today between 45 degrees and 50 degrees S. Holocene climate change in the Amazon tropical rain forest was relatively minor. A reduced north-south migration of the Intertropical Convergence Zone (ITCZ) during the early to middle Holocene is a possible explanation for the synchrony of maximum aridity in the two hemispheres. The mean position of the ITCZ must also have remained more northerly year-round in the early to middle Holocene, reducing easterly moisture throughout South America. Throughout the Americas, the late Holocene was generally wetter and cooler.

DE - DESCRIPTORS: Argentina-; Canada-; Cenozoic-; Central-America; climate-change; Holocene-; lacustrine-environment; Laurentide-ice-sheet; North-America; northern-Canada; paleoclimatology-; paleoecology-; paleogeography-; paleolimnology-; Patagonia-; plains-; Quaternary-; South-America; vegetation-

CC - CATEGORY CODES: 24-Quaternary-geology

DT - DOCUMENT TYPE: Book

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: Refs: 356; illus. incl. 3 tables, sketch map.

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

IB - ISBN: 0-12-472670-4

AN - ACCESSION NUMBER: 2003-061617

UD - UPDATE CODE: 200320

Registro 330 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Le terrane de Slide Mountain (Cordilleres canadiennes); une lithosphere oceanique marquee par des points chauds

Translated Title: Slide Mountain Terrane, Canadian Cordillera; oceanic lithosphere marked by hot spots.

AU - AUTHORS: Tardy-M; Lapierre-H; Bosch-D; Cadoux-A; Narros-A; Struik-L-C; Brunet-P

AF - AUTHOR AFFILIATION: Universite de Savoie, Laboratoire Geodynamique des Chaines Alpines, Le Bourget du Lac, France

SO - SOURCE: Canadian Journal of Earth Sciences = Revue Canadienne des Sciences de la Terre. 40; 6, Pages 833-852. 2003.

PB - PUBLISHER: National Research Council of Canada. Ottawa, ON, Canada. 2003.

CP - COUNTRY OF PUBLICATION: Canada

PY - PUBLICATION YEAR: 2003

LA - LANGUAGE: French

LS - LANGUAGE OF SUMMARY: English

AB - ABSTRACT: The Slide Mountain Terrane consists of Devonian to Permian siliceous and detrital sediments in which are interbedded basalts and dolerites. Locally, ultramafic cumulates intrude these sediments. The Slide Mountain Terrane is considered to represent a back-arc basin related to the Quesnellia Paleozoic arc-terrane. However, the Slide Mountain mafic volcanic rocks exposed in central British Colombia do not exhibit features of back-arc basin basalts (BABB) but those of mid-oceanic ridge (MORB) and oceanic island (OIB) basalts. The N-MORB-type volcanic rocks are characterized by light rare-earth element (LREE)-depleted patterns, La/Nb ratios ranging between 1 and 2. Moreover, their Nd and Pb isotopic compositions suggest that they derived from a depleted mantle source. The within-plate basalts differ from those of MORB affinity by LREE-enriched patterns; higher TiO (sub 2) , Nb, Ta, and Th abundances; lower epsilon (sub Nd) values; and correlatively higher isotopic Pb ratios. The Nd and Pb isotopic compositions of the ultramafic cumulates are similar to those of MORB-type volcanic rocks. The correlations between delta (sub Nd) and incompatible elements suggest that part of the Slide Mountain volcanic rocks derive from the mixing of two mantle sources: a depleted N-MORB type and an enriched OIB type. This indicates that some volcanic rocks of the Slide Mountain basin likely developed from a ridge-centered or near-ridge hotspot. The activity of this hotspot is probably related to the worldwide important mantle plume activity that occurred at the end of Permian times, notably in Siberia.

DE - DESCRIPTORS: back-arc-basins; basalts-; basins-; Canada-; Canadian-Cordillera; chemical-composition; chemical-ratios; concentration-; Devonian-; geochemistry-; hot-spots; igneous-rocks; isotope-ratios; isotopes-; lithosphere-; lithostratigraphy-; mantle-; mantle-plumes; metals-; mid-ocean-ridge-basalts; mixing-; Nd-144-Nd-143; neodymium-; North-America; North-American-Cordillera; ocean-island-basalts; oceanic-lithosphere; Paleozoic-; Permian-; rare-earths; Slide-Mountain-Terrane; stable-isotopes; terranes-; volcanic-rocks; Western-Canada

CC - CATEGORY CODES: 02C-Geochemistry-of-rocks,-soils,-and-sediments; 05A-Igneous-and-metamorphic-petrology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

MC - MAP COORDINATES: LAT: N530000; N540000; LONG: W1213000; W1223000.

IL - ILLUSTRATION: Refs: 33; illus. incl. sects., strat. col., 1 table, sketch maps.

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

IS - ISSN: 0008-4077

CO - CODEN: CJESAP

AN - ACCESSION NUMBER: 2003-057106

UD - UPDATE CODE: 200318

Registro 331 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Influencia del angulo de depresion en la interpretacion geomorfologica de una imagen de SAR

Translated Title: Influence of the depression angles in the geomorphological interpretation of SAR imagery.

AU - AUTHORS: Polidori-Laurent

AF - AUTHOR AFFILIATION: Instituto Geografico "Agustin Codazzi", Bogota, Colombia

BK - BOOK TITLE: In: IV simposio latinoamericano en percepcion remota

Translated Title: IV Latin American symposium on Remote sensing.

BA - BOOK AUTHORS: Pereira-da-Cunha-Roberto (president); Sanchez-Pena-Miguel (chairperson)

SO - SOURCE: Simposio Latinoamericano de Percepcion Remota. 4; Pages 668-676. 1989.

PB - PUBLISHER: SELPER. Bariloche, Argentina. 1989.

CP - COUNTRY OF PUBLICATION: Argentina

PY - PUBLICATION YEAR: 1989

CN - CONFERENCE INFORMATION: IV simposio latinoamericano en percepcion remota. Bariloche, Argentina. Nov. 19-24, 1989.

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English

AB - ABSTRACT: Several SAR images were simulated from a digital elevation model over a 10X15 km test-site of Colombia, with different depression angles. Those simulations were compared in terms of geomorphological information. The shadow and saturation phenomena are very important for that kind of interpretation: their relationship with depression angle was analysed from a theoretical and practical point of view. Some "multi-depression" colour-composites with several configurations were interpreted too.

DE - DESCRIPTORS: digital-terrain-models; erosion-features; geometry-; image-analysis; image-enhancement; imagery-; incidence-angle; interpretation-; landforms-; mapping-; optimization-; physical-properties; pixels-; radar-methods; SAR-; saturation-; simulation-; spatial-data; techniques-; tropical-environment

CC - CATEGORY CODES: 23-Geomorphology; 20-Applied-geophysics

DT - DOCUMENT TYPE: Serial; Conference-Document

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: Refs: 4; illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

CO - CODEN: #06243

AN - ACCESSION NUMBER: 2003-055872

UD - UPDATE CODE: 200318

Registro 332 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Geodynamics of the Northern Andes; subductions and intracontinental deformation (Colombia).

AU - AUTHORS: Taboada-Alfredo; Rivera-Luis; Fuenzalida-Andres; Cisternas-Armando; Philip-Herve; Bijwaard-Harmen; Olaya-Jose; Rivera-Clara

AF - AUTHOR AFFILIATION: Universite de Montpellier II, Laboratoire de Geophysique, Tectonique et Sedimentologie, Montpellier, France

BK - BOOK TITLE: In: AGU 2000 fall meeting.

BA - BOOK AUTHORS: Anonymous

SO - SOURCE: Eos, Transactions, American Geophysical Union. 81; 48, Suppl., Pages 1183. 2000.

PB - PUBLISHER: American Geophysical Union. Washington, DC, United States. 2000.

CP - COUNTRY OF PUBLICATION: United-States

PY - PUBLICATION YEAR: 2000

CN - CONFERENCE INFORMATION: American Geophysical Union 2000 fall meeting. San Francisco, CA, United States. Dec. 15-19, 2000.

LA - LANGUAGE: English

DE - DESCRIPTORS: Andes-; Baudo-Range; Baudo-Panama-island-arc; Choco-Block; Colombia-; compression-tectonics; deformation-; faults-; geodynamics-; Nazca-Plate; Northern-Andes; plate-tectonics; Santa-Marta-Bucaramanga-Fault; South-America; stress-; subduction-; tectonics-

CC - CATEGORY CODES: 16-Structural-geology

DT - DOCUMENT TYPE: Abstract; Serial; Conference-Document

BL - BIB LEVEL: Analytic

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

IS - ISSN: 0096-3941

CO - CODEN: EOSTAJ

AN - ACCESSION NUMBER: 2003-055633

UD - UPDATE CODE: 200318

Registro 333 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Mechanisms of degassing at Nevado del Ruiz Volcano, Colombia.

AU - AUTHORS: Stix-J; Layne-G-D; Williams-S-N

AF - AUTHOR AFFILIATION: McGill University, Department of Earth and Planetary Sciences, Montreal, PQ, Canada

SO - SOURCE: Journal of the Geological Society of London. 160; 4, Pages 507-521. 2003.

PB - PUBLISHER: Geological Society of London. London, United Kingdom. 2003.

CP - COUNTRY OF PUBLICATION: United-Kingdom

PY - PUBLICATION YEAR: 2003

LA - LANGUAGE: English



AB - ABSTRACT: Nevado del Ruiz volcano is an andesite stratovolcano located in the northern Andes of Colombia. The volcano erupted on 11 September 1985, 13 November 1985, and 1 September 1989. The last two eruptions emitted juvenile solid material. This paper examines the volatile and light lithophile trace element contents of melt inclusions and matrix glasses from this juvenile material, and proposes a model for degassing within the volcano. Major element distributions in the glasses show two evolutionary trends, with subsidiary points that lie between the two trends. The data suggest the existence of two separate magmas, which have interacted, mingled, and mixed during their ascent and eruption. Water contents in melt inclusions, as determined by secondary ionization mass spectrometric analysis, are generally low, averaging between 1.6 and 3.3 wt.%. Halogen concentrations in the glasses range from 400 to 1200 ppm for fluorine and from 1100 to 1500 ppm for chlorine. Sulphur contents are low, not exceeding 500 ppm, with most glasses containing <200 ppm. Lithium concentrations range from 20 to 40 ppm, beryllium from 1.5 to 2 ppm, and boron exhibits high variability from 30 to 100 ppm. The only significant difference between melt inclusions and matrix glasses is for water, with matrix glasses having significantly lower concentrations (<0.5 wt.%) than the melt inclusions. The generally elevated concentrations of boron in the magma may be a consequence of enrichment in the source region of the magma, i.e. by subduction of altered oceanic crust and/or sediments. Yet the large degree of boron heterogeneity in both melt inclusions and matrix glasses necessitates subsequent addition of boron at shallower depths as well, by the assimilation of crustal sedimentary rocks or by interaction with hydrothermal fluids. Evidence for pre-eruptive magma emplacement at shallow levels is provided by (1) anhydrous mineral assemblages of plagioclase and pyroxene, (2) high silica contents of glasses, and (3) low water contents in melt inclusions. When combined, these observations suggest a period of magma residence at shallow depths, probably <3 km beneath the summit of the volcano. A multistage model of magma transport and degassing involves alternating periods of magma ascent and magma ponding. Initially, volatile-bearing magma ascends from depths of 9-15 km, driven by buoyancy. During decompression, the magma loses gas, particularly CO (sub 2) and sulphur. The magma eventually ponds at its neutral buoyancy level. At this point, the gas-saturated magma cools and crystallizes, thereby liberating gas under isobaric conditions. As a result, CO (sub 2) is depleted from the magma whereas H (sub 2) O and SiO (sub 2) are enriched. The H (sub 2) O enrichment is caused by its increased solubility in the magma as CO (sub 2) is degassed, whereas SiO (sub 2) is enriched by fractional crystallization. The density of the magma decreases as the level of dissolved H (sub 2) O increases, eventually causing the magma to become buoyant once more and to continue its ascent, either to erupt or to freeze at shallow depths.

DE - DESCRIPTORS: Andes-; andesites-; chemical-composition; Colombia-; concentration-; degassing-; eruptions-; fluid-inclusions; geochemistry-; hybridization-; igneous-rocks; inclusions-; ion-probe-data; magma-transport; magmas-; major-elements; mass-spectra; melt-inclusions; mineral-composition; Nevado-del-Ruiz; Northern-Andes; phenocrysts-; South-America; spectra-; stratovolcanoes-; trace-elements; volatiles-; volcanic-rocks; volcanoes-; water-content

CC - CATEGORY CODES: 02A-General-geochemistry; 24-Quaternary-geology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

MC - MAP COORDINATES: LAT: N045300; N045300; LONG: W0752200; W0752200.

IL - ILLUSTRATION: Refs: 53; illus. incl. 1 table, sketch map.

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute. Reference includes data from The Geological Society, London, London, United Kingdom

IS - ISSN: 0016-7649

CO - CODEN: JGSLAS

AN - ACCESSION NUMBER: 2003-054766

UD - UPDATE CODE: 200318

Registro 334 de 5614 - GeoRef : 2002-2004/12

BK - BOOK TITLE: Tectonic controls on the Late Cretaceous to Cenozoic sedimentary fill of the middle Magdalena Valley basin, Eastern Cordillera and Llanos Basin, Colombia.

BA - BOOK AUTHORS: Gomez-Elias

CP - COUNTRY OF PUBLICATION: United-States

PY - PUBLICATION YEAR: 2001

DG - DEGREE GRANTED: Doctoral

DI - DEGREE GRANTING INSTITUTION: Cornell University. Ithaca, NY, United States. Pages: 649. 2001.

LA - LANGUAGE: English

DE - DESCRIPTORS: Andes-; basin-analysis; Cenozoic-; Colombia-; Cretaceous-; crustal-thickening; Eastern-Cordillera; eustacy-; fission-tracks; geochronology-; lithofacies-; Llanos-; macerals-; Magdalena-Valley; Mesozoic-; patterns-; petroleum-; petroleum-exploration; production-; provenance-; reflectance-; South-America; structural-controls; thermochronology-; unconformities-; Upper-Cretaceous; vitrinite-; volcanic-ash

CC - CATEGORY CODES: 12-Stratigraphy; 29A-Economic-geology,-geology-of-energy-sources

DT - DOCUMENT TYPE: Thesis-or-Dissertation

BL - BIB LEVEL: Monograph

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

IB - ISBN: 0-493-20834-8

AV - AVAILABILITY: University Microfilms, Ann Arbor, MI, United States

AN - ACCESSION NUMBER: 2003-053227

UD - UPDATE CODE: 200317

Registro 335 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Indices de contaminacion para caracterizacion de aguas continentales y vertimientos; formulaciones.

Translated Title: Proposals for pollution indexes to characterize surface waters and watersheds.

AU - AUTHORS: Ramirez-A; Restrepo-R; Cardenosa-M

AF - AUTHOR AFFILIATION: Ecotest, Bogota, Colombia

SO - SOURCE: C.T. and F Ciencia, Tecnologia, Futuro. 1; 5, Pages 89-99. 1999.

PB - PUBLISHER: Ecopetrol. Piedecuesta, Colombia. 1999.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1999

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English

DE - DESCRIPTORS: acidic-composition; aliphatic-hydrocarbons; aromatic-hydrocarbons; biota-; chemical-composition; chemical-waste; Colombia-; drainage-; drainage-basins; hydrocarbons-; hydrology-; industrial-waste; monitoring-; oil-spills; organic-compounds; petroleum-; pH-; pollutants-; pollution-; sampling-; sediments-; South-America; surface-water; temperature-; waste-disposal; water-quality; watersheds-

CC - CATEGORY CODES: 22-Environmental-geology; 02B-Hydrochemistry

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: Refs: 26; illus. incl. 5 tables.

RF - REFERENCE SOURCE: GeoRef, Copyright 2003, American Geological Institute.

IS - ISSN: 0122-5383

AN - ACCESSION NUMBER: 2003-053109

UD - UPDATE CODE: 200317

Registro 336 de 5614 - GeoRef : 2002-2004/12

TI - TITLE: Los paleofluidos en el Grupo Oncala, Cuenca de Cameros (La Rioja, Espana); datos de inclusiones fluidas, isotopos de oxigeno y SEM

Translated Title: Paleofluids in the Oncala Group, Cameros Basin, La Rioja, Spain; data on fluid inclusions, oxygen isotopes and SEM.

AU - AUTHORS: Mantilla-Figueroa-L-C; Casquest-C; Mas-J-R

AF - AUTHOR AFFILIATION: Univ. Ind. Santander, Esc. Geol., Bucaramanga, Colombia

SO - SOURCE: Geogaceta. 24; Pages 207-210. 1998.

PB - PUBLISHER: Sociedad Geologica de Espana. Madrid, Spain. 1998.

CP - COUNTRY OF PUBLICATION: Spain

PY - PUBLICATION YEAR: 1998

CN - CONFERENCE INFORMATION: 24. Sesion Cientifica de la Sociedad Geologica de Espana. Saragossa, Spain. 1998.

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English

DE - DESCRIPTORS: basins-; Berriasian-; calcite-; Cameros-Basin; carbonates-; Cretaceous-; Europe-; fluid-inclusions; framework-silicates; hydrothermal-alteration; Iberian-Peninsula; Iberica-; inclusions-; isotopes-; La-Rioja-Spain; Logrono-City-Spain; Lower-Cretaceous; Mesozoic-; metasomatism-; microthermometry-; Oncala-Group; oxygen-; quartz-; sedimentary-basins; SEM-data; silica-minerals; silicates-; Southern-Europe; Spain-

CC - CATEGORY CODES: 06A-Sedimentary-petrology

DT - DOCUMENT TYPE: Serial; Conference-Document


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