SO - SOURCE: Abstracts with Programs - Geological Society of America. 35; 4, Pages 65. 2003.
PB - PUBLISHER: Geological Society of America (GSA). Boulder, CO, United States. 2003.
CP - COUNTRY OF PUBLICATION: United-States
PY - PUBLICATION YEAR: 2003
CN - CONFERENCE INFORMATION: Geological Society of America, Cordilleran Section, 99th annual meeting. Puerto Vallarta, Mexico. April 1-3, 2003.
LA - LANGUAGE: English
AB - ABSTRACT: In the twenty years since terrane mapping was first applied to Mexico, many of the basic boundaries are similar, however the following advances have been made: (i) subdivision of the composite terranes; (ii) delimitation of the terranes in time; (iii) tectonic interpretation of the geological records; (iv) provision of better constraints on the provenance; and (v) reconstruction of actualistic palinspastic maps from the Mesoproterozoic to the present. In the Precambrian and Paleozoic terranes belong either to North America or Middle America (including Maya, Oaxaquia and Honduras), the latter lying adjacent to Amazonia off Venezuela and Colombia. Outboard of Oaxaquia, lay a Cambro-Ordovician, continental rise prism (Petlalcingo Group) and oceanic lithosphere (Acateco Group). The latter was obducted over the former in the Ordovician and/or Silurian and unconformably overlain by the Tecomate overstep sequence to form the Mixteco terrane. The Sierra Madre terrane lay west of Middle America to which it was accreted in the Ordovician (pebbles of the Sierra Madre occur in Wenlockian strata in Oaxaquia). The Coahuiltecano and Tarahumara terranes represent units lying between North and Middle America. All of these terranes were amalgamated into the supercontinent, Pangea, in the Late Permian. Middle Jurassic breakup of Pangea resulted in two continental blocks, Yucatan and Chortis that were surrounded by small ocean basins: Gulf of Mexico, Caribbean Sea, Juarez and Motagua terranes. In western Mexico, the Guerrero composite terrane consists of oceanic arc and periarc complexes, and equivalent terranes, is transitional into continental lithosphere in southern California. Amalgamation of individual terranes into the Guerrero composite terrane in the mid-Cretaceous may have resulted from collision of Baja British Columbia with the trench. An increased convergence rate between the Farallon and North American plates in the Late Cretaceous and early Tertiary resulted in obduction of the Guerrero composite terrane, the Laramide orogeny, inboard migration of the arc, and amalgamation of all the terranes with North America. Neogene propagation of the East Pacific Rise into the North American margin has led to separation of the Baja California block.
DE - DESCRIPTORS: boundary-conditions; continental-rise; history-; mapping-; Mexico-; obduction-; ocean-floors; paleogeography-; plate-tectonics; provenance-; reconstruction-; tectonics-; terranes-
CC - CATEGORY CODES: 16-Structural-geology
DT - DOCUMENT TYPE: Abstract; Serial; Conference-Document
BL - BIB LEVEL: Analytic
RF - REFERENCE SOURCE: GeoRef, Copyright 2004, American Geological Institute. Reference includes data supplied by the Geological Society of America, Boulder, CO, United States
IS - ISSN: 0016-7592
CO - CODEN: GAAPBC
AN - ACCESSION NUMBER: 2004-012374
UD - UPDATE CODE: 200404
Registro 202 de 5614 - GeoRef : 2002-2004/12
TI - TITLE: Variations in Cascade arc magmatism through space and time; a comparison of geochemical and geographic trends in volcanic and plutonic rocks from the Chilliwack-Mt. Baker and Fifes Peaks-Bumping Lake areas, Washington.
AU - AUTHORS: Tepper-Jeffrey-H; Hammond-Paul-E
AF - AUTHOR AFFILIATION: University of Puget Sound, Tacoma, WA, United States
BK - BOOK TITLE: In: Geological Society of America, Cordilleran Section, 99th annual meeting.
BA - BOOK AUTHORS: Anonymous
SO - SOURCE: Abstracts with Programs - Geological Society of America. 35; 4, Pages 57. 2003.
PB - PUBLISHER: Geological Society of America (GSA). Boulder, CO, United States. 2003.
CP - COUNTRY OF PUBLICATION: United-States
PY - PUBLICATION YEAR: 2003
CN - CONFERENCE INFORMATION: Geological Society of America, Cordilleran Section, 99th annual meeting. Puerto Vallarta, Mexico. April 1-3, 2003.
LA - LANGUAGE: English
AB - ABSTRACT: Volcanic and plutonic rocks of the Cascade arc extend from northern California to British Colombia and preserve a record of subduction-related magmatism over the past approximately 44 Ma. During this interval the arc has experienced variations in several parameters that have the potential to influence magmatism including the rate of subduction, the age and volatile content of the subducting plate, and the stress regime, thickness and composition of the overlying continental crust. This study compares spatial and temporal patterns of magmatic activity in two areas of the Washington Cascades with the goals of: (1) identifying trends that may be related to changing subduction parameters, and (2) contrasting the records of plutonic versus volcanic rocks. The two areas under study are the Chilliwack-Mt. Baker area (CMB), which includes >40 plutons of the Chilliwack batholith (35 Ma to <3 Ma), and the Fifes Peaks-Bumping Lake area (FPBL), which contains over 46 dated volcanic and plutonic units (32 Ma to Recent). In both areas the interval 27-22 Ma was marked by voluminous activity that included emplacement of distinctive leucocratic granitoids indicative of hydrous melting. Both areas then experienced a hiatus ( approximately 22-12 Ma) after which magmatism resumed but was different in character. In the CMB magmatism since 12 Ma is confined to a NE-trending belt within which there is a younger-to-the-SW progression. Plutons in this belt generally have lower Ba/Nb, lower B/Be, higher incompatible element concentrations (e.g., Nb, Th), and smaller areas than the older plutons. These differences may reflect declining fluid flux from the slab (and decreased melting) as the rate of subduction slowed. In the FPBL the hiatus was followed (11-2 Ma) by emplacement of hornblende dacites that have adakite traits (e.g., Sr/Y > 40, Y < 15 ppm) and define a younger-to-the-SE progression. The presence of adakites in the FPBL but not the CMB may reflect a difference between the two areas in the age of the subducting slab. Preliminary results of this study suggest that many of the temporal and spatial trends observed in CMB and FPBL are strongly influenced by local variations in subduction parameters including slab age and geometry.
DE - DESCRIPTORS: Bumping-Lake; Cascade-Range; Chilliwack-Batholith; Chilliwack-River; continental-crust; crust-; emplacement-; Fifes-Peaks; igneous-rocks; intrusions-; magmatism-; mineral-composition; Mount-Baker; plate-tectonics; plutonic-rocks; plutons-; slabs-; subduction-; United-States; volcanic-rocks; volcanoes-; Washington-
CC - CATEGORY CODES: 18-Solid-earth-geophysics; 05A-Igneous-and-metamorphic-petrology
DT - DOCUMENT TYPE: Abstract; Serial; Conference-Document
BL - BIB LEVEL: Analytic
RF - REFERENCE SOURCE: GeoRef, Copyright 2004, American Geological Institute. Reference includes data supplied by the Geological Society of America, Boulder, CO, United States
IS - ISSN: 0016-7592
CO - CODEN: GAAPBC
AN - ACCESSION NUMBER: 2004-012330
UD - UPDATE CODE: 200404
Registro 203 de 5614 - GeoRef : 2002-2004/12
TI - TITLE: Neogene marine mollusks in Baja California and the ancient Gulf of California have Holocene and fossil records in the Caribbean province.
AU - AUTHORS: Smith-Judith-Terry
AF - AUTHOR AFFILIATION: 2330 14th Street North, 1, Arlington, VA, United States
BK - BOOK TITLE: In: Geological Society of America, Cordilleran Section, 99th annual meeting.
BA - BOOK AUTHORS: Anonymous
SO - SOURCE: Abstracts with Programs - Geological Society of America. 35; 4, Pages 28. 2003.
PB - PUBLISHER: Geological Society of America (GSA). Boulder, CO, United States. 2003.
CP - COUNTRY OF PUBLICATION: United-States
PY - PUBLICATION YEAR: 2003
CN - CONFERENCE INFORMATION: Geological Society of America, Cordilleran Section, 99th annual meeting. Puerto Vallarta, Mexico. April 1-3, 2003.
LA - LANGUAGE: English
AB - ABSTRACT: High tech methodologies and theoretical models currently prevail in paleogeographic reconstructions of complex plate boundary areas, but low tech, collections-based paleontological research provides a time frame for tectonostratigraphic events and the geographic connections between marine embayments and plate slivers. Updated nomenclature for Pacific and Caribbean, Holocene and fossil index species and subspecies is critical because the same taxon may have multiple names for living and fossil specimens from different basins. Taxonomic splitting obscures conspecific and phylogenetic relationships that indicate distribution patterns in time and space, and that correlate sediments along the complex Pacific/North American Plate boundary. This area includes the southwestern Basin and Range Province, southern San Andreas Fault system, Gulf Extensional Province, the northern East Pacific Rise and the California Continental Borderland. Tertiary marine fossils from Baja California and the Salton Trough of California have newly refined ages based on associated radiometrically-dated volcanic rocks. They correlate particular embayments in west Mexico and southern California with classic sections in Panama, Costa Rica, Dominican Republic, Trinidad, Venezuela, Colombia and Ecuador. They also relate western Baja California to slivers of tectonic terranes in southern California. Field work and the extensive Paleobiology and Systematic Biology collections in the Smithsonian Institution's National Museum of Natural History provide comparative data on molluscan biodiversity, morphologic variability, geographic distributions and ecology. Work in progress suggests that some taxa are time-transgressive: early Middle to Late Miocene age in west Mexico and the ancient Gulf of California, Miocene, undifferentiated in Panama, Colombia, Venezuela, and Trinidad, and living in the eastern Caribbean. Attention to specific and subspecific nomenclature will greatly improve Bioinformatics databases that aim to include all organisms, living and fossil, world-wide.
DE - DESCRIPTORS: Baja-California; biogeography-; Caribbean-region; Cenozoic-; continental-borderland; East-Pacific; faunal-provinces; Gulf-of-California; Holocene-; index-fossils; Invertebrata-; marine-environment; Mexico-; Mollusca-; Neogene-; North-Pacific; Northeast-Pacific; Pacific-Ocean; paleogeography-; Quaternary-; reconstruction-; Tertiary-
CC - CATEGORY CODES: 12-Stratigraphy
DT - DOCUMENT TYPE: Abstract; Serial; Conference-Document
BL - BIB LEVEL: Analytic
RF - REFERENCE SOURCE: GeoRef, Copyright 2004, American Geological Institute. Reference includes data supplied by the Geological Society of America, Boulder, CO, United States
IS - ISSN: 0016-7592
CO - CODEN: GAAPBC
AN - ACCESSION NUMBER: 2004-012299
UD - UPDATE CODE: 200404
Registro 204 de 5614 - GeoRef : 2002-2004/12
TI - TITLE: Mid-Jurassic tectonothermal event superposed on a Paleozoic geological record in the Acatlan Complex of southern Mexico; hotspot activity during the breakup of Pangea.
AU - AUTHORS: Keppie-J-D; Nance-R-D; Dostal-J; Ortega-Rivera-Amabel; Miller-B-V
AF - AUTHOR AFFILIATION: Universidad Nacional Autonoma de Mexico, Mexico City, Mexico
BK - BOOK TITLE: In: Geological Society of America, Cordilleran Section, 99th annual meeting.
BA - BOOK AUTHORS: Anonymous
SO - SOURCE: Abstracts with Programs - Geological Society of America. 35; 4, Pages 23. 2003.
PB - PUBLISHER: Geological Society of America (GSA). Boulder, CO, United States. 2003.
RP - RESEARCH PROGRAM: IGCP (International Geological Correlation Programme)
CP - COUNTRY OF PUBLICATION: United-States
PY - PUBLICATION YEAR: 2003
CN - CONFERENCE INFORMATION: Geological Society of America, Cordilleran Section, 99th annual meeting. Puerto Vallarta, Mexico. April 1-3, 2003.
LA - LANGUAGE: English
AB - ABSTRACT: U-Pb and 40Ar/39Ar isotopic analyses of various minerals from the lowest structural units of the Acatlan Complex of southern Mexico indicate that low pressure migmatization (5-6 kb), polyphase deformation, and intrusion of felsic and mafic magmas all occurred between 175+ or -3 Ma and 171+ or -1 Ma, i.e. mid-Jurassic. These effects are superimposed upon Ordovician-Silurian and Permian tectonothermal events reflected in older age data in the northern part of the Acatlan Complex. Fractionation of olivine and bronzite in the mafic magmas was associated with assimilation of alumina producing layered lower crustal intrusions of cumulitic dunites, gabbro, and norite that are cut by appinitic dykes. Ensuing rapid cooling through 350 degrees , 280 degrees and 150 degrees C by 167+ or -2 Ma, 166+ or -2 Ma, and 160+ or -14 Ma, respectively, accompanied rapid exhumation (up to 10 km/my), and was followed by deposition of Middle Jurassic (Bajocian=166-160 Ma) sediments. The Jurassic uplift is consistent with the top-to-the west tectonic unroofing inferred to have occurred during the Main phase of deformation. Synchronous tectonic unroofing is also recorded in the adjacent Oaxaca terrane, 100 km to the east, where top-to-the-north, extensional shear zones occur in Paleozoic strata. This pattern of extension suggests radial tectonic unroofing in response to domal uplift (radius >100 km) like that associated with core complexes, slab windows, and hotspots. Most tectonic analyses for the Jurassic place the Acatlan Complex in the forearc region of an arc lying 600-800 km inboard of the subduction zone in Colombia, presumably in response to flat-slab subduction. Modern analogues suggest that flat-slab subduction reflects subduction of young buoyant oceanic lithosphere adjacent to either a mid-oceanic ridge, or a plume. Since core complexes are typical of arc-backarc regions, and slab windows generally produce metamorphic belts, the forearc setting and associated domal uplift suggest a plume to be the most likely cause of this Jurassic tectonothermal pulse in southern Mexico. This plume activity is synchronous with the opening of the Gulf of Mexico during the breakup of Pangea, to which it may have contributed.
DE - DESCRIPTORS: absolute-age; Acatlan-Complex; Ar-Ar; dates-; deformation-; dikes-; hot-spots; IGCP-; intrusions-; Jurassic-; magmatism-; Mesozoic-; metamorphism-; Mexico-; Middle-Jurassic; migmatization-; paleogeography-; Paleozoic-; Pangaea-; plate-tectonics; polyphase-processes; southern-Mexico; subduction-; U-Pb; uplifts-
CC - CATEGORY CODES: 18-Solid-earth-geophysics
DT - DOCUMENT TYPE: Abstract; Serial; Conference-Document
BL - BIB LEVEL: Analytic
NN - ANNOTATION: IGCP Project No. 453.
RF - REFERENCE SOURCE: GeoRef, Copyright 2004, American Geological Institute. Reference includes data supplied by the Geological Society of America, Boulder, CO, United States
IS - ISSN: 0016-7592
CO - CODEN: GAAPBC
AN - ACCESSION NUMBER: 2004-012268
UD - UPDATE CODE: 200404
Registro 205 de 5614 - GeoRef : 2002-2004/12
BK - BOOK TITLE: FS Sonne Fahrtbericht SO 159/ cruise report Salieri "South American lithospheric transects across volcanic ridges"; Guayaquil-Guayaquil, August 21-September 17, 2001.
BA - BOOK AUTHORS: Flueh-Ernst-R (editor); Bialas-Joerg (editor); Charvis-Philippe (editor)
SO - SOURCE: GEOMAR-Report. 101; 2001.
PB - PUBLISHER: GEOMAR, Forschungszentrum fur Marine Geowissenschaften der Christian-Albrechts-Universitaet zu Keil. Kiel, Federal Republic of Germany. Pages: 256. 2001.
CP - COUNTRY OF PUBLICATION: Federal-Republic-of-Germany
PY - PUBLICATION YEAR: 2001
LA - LANGUAGE: English
LS - LANGUAGE OF SUMMARY: German; French
DE - DESCRIPTORS: Colombia-; continental-margin; East-Pacific; echo-sounding; Ecuador-; geophysical-methods; geophysical-profiles; geophysical-surveys; geotraverses-; lithosphere-; magnetic-anomalies; magnetic-methods; mid-ocean-ridges; ocean-basins; ocean-floors; Pacific-Ocean; seismic-methods; seismic-profiles; South-America; South-Pacific; Southeast-Pacific; surveys-
CC - CATEGORY CODES: 07-Oceanography; 20-Applied-geophysics
DT - DOCUMENT TYPE: Serial
BL - BIB LEVEL: Monograph
MC - MAP COORDINATES: LAT: S033000; N020000; LONG: W0800000; W0850000.
IL - ILLUSTRATION: illus. incl. tables, sects., sketch maps.
RF - REFERENCE SOURCE: GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Geoline, Bundesanstalt fur Geowissenschaften und Rohstoffe, Hanover, Germany
IS - ISSN: 0936-5788
AN - ACCESSION NUMBER: 2004-012123
UD - UPDATE CODE: 200404
Registro 206 de 5614 - GeoRef : 2002-2004/12
TI - TITLE: Amonitas del Barremiano en Villa de Leyva, Boyaca (Colombia, Sur America); datos bioestratigraficos preliminares
Translated Title: Barremian Ammonites from Leyva, Boyaca, Colombia, South America; preliminary biostratigraphic data.
AU - AUTHORS: Patarroyo-Pedro
AF - AUTHOR AFFILIATION: Universidad Nacional de Colombia, Bogota, Colombia
BK - BOOK TITLE: In: 16th Latin American geoscientific colloquium.
BA - BOOK AUTHORS: Veit-H (editor); Grosjean-Martin (editor); Miller-H (editor); Rosenfeld-U (editor)
SO - SOURCE: Zentralblatt fuer Geologie und Palaeontologie, Teil I: Allgemeine, Angewandte, Regionale und Historische Geologie. 1999; 7-8, Pages 789-798. 2000.
PB - PUBLISHER: E. Schweizerbart'sche Verlagsbuchhandlung. Stuttgart, Federal Republic of Germany. 2000.
CP - COUNTRY OF PUBLICATION: Federal-Republic-of-Germany
PY - PUBLICATION YEAR: 2000
CN - CONFERENCE INFORMATION: 16th Latin American geoscientific colloquium. Bayreuth, Federal Republic of Germany. Oct. 14, 1998.
LA - LANGUAGE: Spanish
LS - LANGUAGE OF SUMMARY: English; German
DE - DESCRIPTORS: Ammonites-; Ammonoidea-; Barremian-; biostratigraphy-; Boyaca-Colombia; Cephalopoda-; Colombia-; Cretaceous-; cross-sections; Invertebrata-; Leyva-Colombia; Lower-Cretaceous; Mesozoic-; Mollusca-; South-America; stratigraphic-boundary; stratigraphic-columns; Tetrabranchiata-
CC - CATEGORY CODES: 12-Stratigraphy; 10-Invertebrate-paleontology
DT - DOCUMENT TYPE: Serial; Conference-Document
BL - BIB LEVEL: Analytic
IL - ILLUSTRATION: Refs: 25; sect., strat. col., sketch map.
RF - REFERENCE SOURCE: GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Geoline, Bundesanstalt fur Geowissenschaften und Rohstoffe, Hanover, Germany
IS - ISSN: 0340-5109
IB - ISBN: 3-510-66021-8
CO - CODEN: ZGPAAK
AN - ACCESSION NUMBER: 2004-011729
UD - UPDATE CODE: 200404
Registro 207 de 5614 - GeoRef : 2002-2004/12
TI - TITLE: Structural style and amount of shortening of the folded Bogota segment, Eastern Cordillera of Colombia.
AU - AUTHORS: Kammer-Andreas; Mora-Andres
AF - AUTHOR AFFILIATION: Universidad Nacional de Colombia, Bogota, Colombia
BK - BOOK TITLE: In: 16th Latin American geoscientific colloquium.
BA - BOOK AUTHORS: Veit-H (editor); Grosjean-Martin (editor); Miller-H (editor); Rosenfeld-U (editor)
SO - SOURCE: Zentralblatt fuer Geologie und Palaeontologie, Teil I: Allgemeine, Angewandte, Regionale und Historische Geologie. 1999; 7-8, Pages 823-837. 2000.
PB - PUBLISHER: E. Schweizerbart'sche Verlagsbuchhandlung. Stuttgart, Federal Republic of Germany. 2000.
CP - COUNTRY OF PUBLICATION: Federal-Republic-of-Germany
PY - PUBLICATION YEAR: 2000
CN - CONFERENCE INFORMATION: 16th Latin American geoscientific colloquium. Bayreuth, Federal Republic of Germany. Oct. 14, 1998.
LA - LANGUAGE: English
LS - LANGUAGE OF SUMMARY: German; Spanish
DE - DESCRIPTORS: Andean-Orogeny; Andes-; Bogota-Colombia; Cenozoic-; Colombia-; cross-sections; crustal-shortening; Eastern-Cordillera; folds-; models-; Neogene-; Pliocene-; South-America; style-; tectonics-; Tertiary-
CC - CATEGORY CODES: 16-Structural-geology
DT - DOCUMENT TYPE: Serial; Conference-Document
BL - BIB LEVEL: Analytic
IL - ILLUSTRATION: Refs: 17; sects., 1 table, geol. sketch map.
RF - REFERENCE SOURCE: GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Geoline, Bundesanstalt fur Geowissenschaften und Rohstoffe, Hanover, Germany
IS - ISSN: 0340-5109
IB - ISBN: 3-510-66021-8
CO - CODEN: ZGPAAK
AN - ACCESSION NUMBER: 2004-011727
UD - UPDATE CODE: 200404
Registro 208 de 5614 - GeoRef : 2002-2004/12
TI - TITLE: Metamorphic evolution of the pre-Silurian rocks of the Santander Massif, Colombia, South America.
AU - AUTHORS: Barragan-M; Montenegro-G
AF - AUTHOR AFFILIATION: Universidad Industrial de Santander, Escuela de Geologia, Bucaramanga, Colombia
BK - BOOK TITLE: In: Brazil 2000; 31st international geological congress; abstracts volume.
BA - BOOK AUTHORS: Anonymous
SO - SOURCE: International Geological Congress, Abstracts = Congres Geologique International, Resumes. 31; Pages ; unpaginated. 2000.
PB - PUBLISHER: [International Geological Congress]. [location varies], International. 2000.
RP - RESEARCH PROGRAM: IGC (International Geological Congress)
CP - COUNTRY OF PUBLICATION: International
PY - PUBLICATION YEAR: 2000
CN - CONFERENCE INFORMATION: Brazil 2000; 31st international geological congress. Rio de Janeiro, Brazil. Aug. 6-17, 2000.
LA - LANGUAGE: English
DE - DESCRIPTORS: Bucaramanga-Formation; Caledonian-Orogeny; Colombia-; deformation-; dynamic-metamorphism; exhumation-; facies-; foliation-; gneisses-; lower-Paleozoic; magmatism-; metamorphic-rocks; metamorphism-; mineral-assemblages; orthogneiss-; P-T-conditions; Paleozoic-; plate-collision; plate-tectonics; retrograde-metamorphism; Santander-Colombia; schistosity-; South-America; structural-analysis; style-; thermal-metamorphism
CC - CATEGORY CODES: 05A-Igneous-and-metamorphic-petrology
DT - DOCUMENT TYPE: Abstract; Serial; Conference-Document
BL - BIB LEVEL: Analytic
MC - MAP COORDINATES: LAT: N054500; N080800; LONG: W0722000; W0743000.
NN - ANNOTATION: File G1002013.PDF.
ME - SOURCE MEDIUM: compact disc
RF - REFERENCE SOURCE: GeoRef, Copyright 2004, American Geological Institute.
CO - CODEN: IGABBY
AN - ACCESSION NUMBER: 2004-010296
UD - UPDATE CODE: 200404
Registro 209 de 5614 - GeoRef : 2002-2004/12
TI - TITLE: Geological and structural characteristics in and around the La Merced marble layers, Central Cordillera of the Colombian Andes.
AU - AUTHORS: Gil-Escobar-F-A
AF - AUTHOR AFFILIATION: Shimane University, Matsue, Japan
BK - BOOK TITLE: In: Brazil 2000; 31st international geological congress; abstracts volume.
BA - BOOK AUTHORS: Anonymous
SO - SOURCE: International Geological Congress, Abstracts = Congres Geologique International, Resumes. 31; Pages ; unpaginated. 2000.
PB - PUBLISHER: [International Geological Congress]. [location varies], International. 2000.
RP - RESEARCH PROGRAM: IGC (International Geological Congress)
CP - COUNTRY OF PUBLICATION: International
PY - PUBLICATION YEAR: 2000
CN - CONFERENCE INFORMATION: Brazil 2000; 31st international geological congress. Rio de Janeiro, Brazil. Aug. 6-17, 2000.
LA - LANGUAGE: English
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