No. Registros Solicitud 1 5614 colombia



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DE - DESCRIPTORS: chemistry-; Colombia-; igneous-rocks; petrology-; rock-analyses; South-America

CC - CATEGORY CODES: 05-Igneous-and-metamorphic-petrology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

AN - ACCESSION NUMBER: 1963-004383

UD - UPDATE CODE: 1963

Registro 2880 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Consideraciones sobre el estado actual de la estratigrafa del terciario en Colombia.

AU - AUTHORS: Porta-Jaime-de

SO - SOURCE: Boletin de Geologia (Bucaramanga). 9; Pages 5-43. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English; French

AB - ABSTRACT: The stratigraphy of the marine and continental Tertiary in Colombia has been established on the basis of a few isolated sections that represent the chronostratigraphy used in Europe. A review of the main points of stratigraphy shows inconsistencies and lack of correlation with the stratigraphic data recently published in the Caribbean region and Europe. The lowering of the Oligocene-Miocene boundary in the Caribbean means a reduction of the Oligocene. Ages and correlations deduced from palynological analysis are founded on a marine sequence. If the marine sediments which formerly were middle and upper Oligocene belong now to the Miocene, the same would happen to their respective continental sediments. However, this is contradictory with the upper Oligocene mammalian fauna. Therefore it is difficult to establish, with reference to the composite palynological diagram of Colombia, what part of the old Oligocene is acceptable as Miocene, and as middle and upper Oligocene. In the marine Tertiary, therefore, correlations are established with the planktonic foraminiferal zones of Stainforth. Under present conditions a complete review of the stratigraphy of the marine and continental Tertiary including transgressions, regressions, sedimentary cycles, and tectonic phases is necessary.

DE - DESCRIPTORS: Caribbean-and-European-correlations; Cenozoic-; Colombia-; Foraminifera-; Invertebrata-; microfossils-; Protista-; regional-; regional-Caribbean-and-European-correlations; South-America; stratigraphic-range-and-correlations; stratigraphy-; Tertiary-

CC - CATEGORY CODES: 12-Stratigraphy

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-002622

UD - UPDATE CODE: 1967

Registro 2881 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Interferencia de direcciones en los pliegues cretacico-terciarios entre Coello y Gualanday.

AU - AUTHORS: Tellez-N-I; Navas-G-J

SO - SOURCE: Boletin de Geologia (Bucaramanga). 9; Pages 45-61. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English; French

AB - ABSTRACT: The western area of a portion of the upper Magdalena valley between Gualanday, Coello, and Doima, in the department of Tolima (Colombia), contains the Guaduas and Gualanday formations. These continental units of Paleocene to Oligocene age respectively total about 1150 meters and are composed principally of variegated shales, sandstones, and conglomerates. In the eastern part of the area limestone, shales, and sandstones of Coniacian to Maestrichtian age are exposed. There is apparently a difference between folding of the Cretaceous and lower Tertiary sequence and folds in the upper Gualanday sequence. The former trend north-northeast and the latter due north. Local angular and progressive unconformities are a result of this difference. There is also opposition of anticlines with synclines and lack of structural continuity. Although the north trend dominates in some cases, the older direction is still maintained in folds of some younger strata so that there is apparent interference between these two directions.

DE - DESCRIPTORS: Cenozoic-; Colombia-; Cretaceous-; Cretaceous-and-Tertiary-structures; folds-; interference-of-directions; Magdalena-Valley; Mesozoic-; South-America; structural-geology; Superposed-; Tertiary-

CC - CATEGORY CODES: 16-Structural-geology

DT - DOCUMENT TYPE: Serial; Map

BL - BIB LEVEL: Analytic

MS - MAP SCALE: 1:50,000

IL - ILLUSTRATION: illus. incl. colored geol. map .

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-002623

UD - UPDATE CODE: 1967

Registro 2882 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Comprobacion biometrica de las especies Codakia orbicularis y Codakia orbiculata.

AU - AUTHORS: Etayo-F

SO - SOURCE: Boletin de Geologia (Bucaramanga). 9; Pages 63-67. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English; French

AB - ABSTRACT: This study quantitatively compares the morphological character of two populations of pelecypods which were separated as two species. The species are Codakia orbicularis Linne and C. orbiculata Montagu. A triangular diagram was constructed using as apical points: length along the antero-posterior line; length of the lunule; and diameter along the antero-posterior line. The two species plot in distinctly different portions of the diagram, and on this basis the author interprets the pelecypods as being of two different species.

DE - DESCRIPTORS: biometrics-; Bivalvia-; Cenozoic-; Codakia-; Colombia-; Invertebrata-; Mollusca-; morphology-; paleontology-; Pleistocene-; Quaternary-; South-America; species-distinction; Tierrabomba-island

CC - CATEGORY CODES: 10-Invertebrate-paleontology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-002624

UD - UPDATE CODE: 1967

Registro 2883 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Discusion sobre las edades de las formaciones Hoyon, Gualanday y La Cira en la region de Honda-San Juan de Rioseco.

AU - AUTHORS: Porta-Jaime-de; Sole-de-Porta-N

SO - SOURCE: Boletin de Geologia (Bucaramanga). 9; Pages 69-85. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

AB - ABSTRACT: Results obtained from analytical pollen studies of the Hoyon, Gualanday, and La Cira formations in the Honda area of the Magdalena valley (Colombia) yield a series of stratigraphic problems similar to those discovered in recent studies of the Caribbean region. Study of the palynological diagram of Colombia indicates that their foundation is suspect and the geochronologic meaning is questionable. Pollen from the base of the Hoyon formation contains elements of the Cicatricosisporites group which according to Van der Hammen appears only in the lower Oligocene, indicating a lower Oligocene age for this formation rather than lower Eocene. Considering the Tertiary stratigraphy of this area it is difficult to relate the Gualanday formation at its type locality to what has been termed the Gualanday formation in the San Juan de Rioseco area. The La Cira formation is provisionally considered to be of Miocene age. Because of these difficulties it is best to consider as a whole the pollen groups of each formation, without assigning an age to it, until it is possible to establish one stratigraphy based on the presence or absence of a group of species.

DE - DESCRIPTORS: Cenozoic-; Colombia-; Gualanday-and-La-Cira-formations; Honda-Jerusalen-region; Hoyon-; microfossils-; palynomorphs-; range-; South-America; stratigraphy-; Tertiary-

CC - CATEGORY CODES: 12-Stratigraphy

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-002625

UD - UPDATE CODE: 1967

Registro 2884 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Geologa del carbonfero al N. de Bucaramanga.

AU - AUTHORS: Navas-G-J

SO - SOURCE: Boletin de Geologia (Bucaramanga). 11; Pages 23-32. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English; French

AB - ABSTRACT: This study of the Carboniferous beds north of Bucaramanga covers the area limited on the east and west by the Bucaramanga and Suarez-Ro de Oro faults respectively. The beds which correspond to the Surata series are divisible into three parts. The lower portion consists of 90 m of reddish sandstones and quartzites generally fine-grained, but with occasional pebbles of quartz. The middle unit, 360 m thick, is composed of limestones at the base, red and gray shales in the center, and limestone conglomerates and claystone at the top. The lower limestones are used in the manufacture of cement. The upper unit is composed of 95 m of gray shales and claystones that are locally arenaceous and calcareous. Structurally the region forms the east flank of an anticline that trends north-northwest. Dips range between 40-70 degrees to the east.

DE - DESCRIPTORS: Bucaramanga-; Carboniferous-; Colombia-; Paleozoic-; South-America; stratigraphy-

CC - CATEGORY CODES: 12-Stratigraphy

DT - DOCUMENT TYPE: Serial; Map

BL - BIB LEVEL: Analytic

MS - MAP SCALE: 1:20,000

IL - ILLUSTRATION: illus. incl. colored geol. map .

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-003554

UD - UPDATE CODE: 1967

Registro 2885 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: La estratigrafa de la formacion Guadalupe y las estructuras por gravedad en la serrana de Cha (Sabana de Bogota).

AU - AUTHORS: Julivert-M

SO - SOURCE: Boletin de Geologia (Bucaramanga). 11; Pages 5-21. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

AB - ABSTRACT: The Guadalupe formation outcrops in the Cha hills area on the Bogota plateau. It is divisible in four units which from oldest to youngest are: the Raizal member ('indurated' sandstone) 200 m thick; the Plaeners horizon 100 m thick of shale, porcelanites, and minor sandstones; the Hard sandstone 70 m thick; and the Soft sandstone 50 m thick. Ten meters of shales and porcelanites occur between the Hard and Soft sandstone. Thickness and lithology of the Guadalupe in the Cha area are similar to those in other parts of the Bogota plateau indicating an extensive single depositional basin. The Cha hills are formed by a tight anticline, but only the eastern limb is developed in the northern half of this range. Gravity collapse structures are developed on the anticline, especially on the eastern limb. These structures were produced by sliding of beds down the dip of the beds of the Plaeners horizon. Dips of 35-60 degrees favor sliding. Gravity sliding is confined principally to the flanks of those folds where the overlying sandstones have been removed by erosion and there is no longer a buttress to support the incompetent shales and porcelanites which then collapse gravitationally.

DE - DESCRIPTORS: Bogota-; Bogota-plateau; Colombia-; gravity-; Guadalupe-; Paleozoic-; Permian-; South-America; stratigraphy-; tectonics-

CC - CATEGORY CODES: 12-Stratigraphy; 16-Structural-geology

DT - DOCUMENT TYPE: Serial; Map

BL - BIB LEVEL: Analytic

MS - MAP SCALE: 1:75,000

IL - ILLUSTRATION: illus. incl. colored geol. map .

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-003555

UD - UPDATE CODE: 1967

Registro 2886 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Sur un bois fossile du Departement de Bolivar (Colombie).

AU - AUTHORS: Boureau-Edouard; Salard-Marguerite

SO - SOURCE: Boletin de Geologia (Bucaramanga). 11; Pages 35-42. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: French

AB - ABSTRACT: A specimen of wood was collected near Palmitos in the Department of Bolvar, Colombia. The specimen was from the upper part of a series of conglomerates and gravels 150-200 m thick, apparently of deltaic origin. The beds are related to Pliocene mammal-bearing beds 30 km south of Palmitos. The specimen is silicified and the colors vary from beige to red. It is identified as Ficoxylon cretaceum and a detailed description and list of affinities are presented.

DE - DESCRIPTORS: Angiospermae-; Bolvar-; Cenozoic-; Colombia-; Neogene-; paleontology-; Plantae-; Pliocene-; South-America; Spermatophyta-; Tertiary-

CC - CATEGORY CODES: 09-Paleobotany

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-003556

UD - UPDATE CODE: 1967

Registro 2887 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Micropaleontologa del cretacico al NW de Bogota (Colombia).

AU - AUTHORS: Colom-G

SO - SOURCE: Boletin de Geologia (Bucaramanga). 10; Pages 69-80. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English; French

AB - ABSTRACT: Seventeen samples were collected from Cretaceous beds between Bogota and Guaduas. The beds sampled range in age from upper Hauterivian to lower Campanian (Cretaceous). Detailed petrologic and petrographic descriptions are given for each sample and the microfossil content is determined. In the Hauterivian beds, terrigenous materials are dominant. In the middle Albian, Radiolaria occur in limy shales indicating conditions of marine deposition in a pelagic environment. In the Turonian and Coniacian, benthonic foraminifera occur in littoral limy marls which alternate with beds indicative of pelagic conditions. Pelagic deposits in the Bogota region are believed not to represent conditions of great depth.

DE - DESCRIPTORS: Bogota-Guaduas-area; Colombia-; Cretaceous-; Foraminifera-and-Radiolaria; Hauterivian-Campanian; Invertebrata-; Mesozoic-; microfossils-; paleontology-; Protista-; South-America

CC - CATEGORY CODES: 10-Invertebrate-paleontology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-003600

UD - UPDATE CODE: 1967

Registro 2888 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Estudio petrografico de la parte alta de la formacion Guadalupe (cretacico superior) al E de Bogota.

AU - AUTHORS: Zamarreno-de-Julivert-I

SO - SOURCE: Boletin de Geologia (Bucaramanga). 10; Pages 55-67. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

AB - ABSTRACT: A petrographic study of 115 samples of the Hard and Soft sandstones of the upper Cretaceous Guadalupe formation collected near Bogota, Colombia, shows significant differences between the units. The Hard sandstone, the lower unit, is characterized by the presence of glauconite in most of the section, by the presence of abundant matrix in some layers, and by lower median size values of quartz grains. The nature of the cement is variable with development of much carbonate cement and a greater amount of ferruginous cement. The Soft sandstone, the upper unit, is characterized by low glauconite content, high median size values of quartz grains, and abundance of quartzitic texture. Kaolinite is abundant in the cement and calcium carbonate cement is rare.

DE - DESCRIPTORS: Bogota-area; clastic-rocks; Colombia-; Cretaceous-; Guadalupe-formation; hard-and-soft; Mesozoic-; petrology-; sandstone-; sedimentary-petrology; sedimentary-rocks; South-America; upper-

CC - CATEGORY CODES: 05-Igneous-and-metamorphic-petrology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-003601

UD - UPDATE CODE: 1967

Registro 2889 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Estudio sedimentologico de la parte alta de la formacion Guadalupe al E de Bogota (cretacico superior).

AU - AUTHORS: Julivert-M

SO - SOURCE: Boletin de Geologia (Bucaramanga). 10; Pages 25-54. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

AB - ABSTRACT: The sedimentological characteristics of the Hard and Soft sandstones from the upper part of the Guadalupe formation near Bogota, Colombia, are described. The Hard sandstone, the lower unit, is composed of about 65 m of thick beds separated by layers of finer material; the mean grain size in the sandstone beds is about 0.25 mm. The Soft sandstone, the upper unit, is composed of about 50 m of cross-bedded and ripple-marked sandstone of medium to coarse grain (0.25-1.0 mm). Cumulative curves of both sandstones are similar as both are well sorted with little asymmetry but they form two separate groups. The Soft sandstone has a more restricted grain size. Between the Soft and Hard sandstone are 16 m of clay, silt, and very fine sandstone. The presence of calcite cement in the Hard sandstone also serves to distinguish it from the Soft sandstone in the field. Petrographically both sandstones are orthoquartzites. The Hard sandstone was deposited under uniform conditions. The Soft sandstone was deposited under more variable conditions and the direct influence of currents. This is due to shoaling of the area which ultimately culminated in deposition of coal and continental sediments after formation of the Soft sandstone.

DE - DESCRIPTORS: Bogota-area; clastic-rocks; Colombia-; Cretaceous-; Guadalupe-formation; hard-and-soft; hard-and-soft-sandstone; Mesozoic-; petrology-; sandstone-; sedimentary-petrology; sedimentary-rocks; South-America; uniform-and-variable-conditions

CC - CATEGORY CODES: 05-Igneous-and-metamorphic-petrology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus. incl. sketch map.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

IS - ISSN: 0120-0283

CO - CODEN: UISBAV

AN - ACCESSION NUMBER: 1967-003602

UD - UPDATE CODE: 1967

Registro 2890 de 5614 - GeoRef Disc 1: 1785-1974

TI - TITLE: Edentata Xenarthra del mioceno de La Venta (Colombia); 1, Dasypodoidea y Glyptodontoidea.

AU - AUTHORS: Porta-Jaime-de

SO - SOURCE: Boletin de Geologia (Bucaramanga). 10; Pages 5-19. 1962.

PB - PUBLISHER: Universidad Industrial de Santander. Bucaramanga, Colombia. 1962.

CP - COUNTRY OF PUBLICATION: Colombia

PY - PUBLICATION YEAR: 1962

LA - LANGUAGE: Spanish

LS - LANGUAGE OF SUMMARY: English; French

AB - ABSTRACT: The presence of edentates in the abundant faunas of the Miocene of the La Venta area, Villavieja, department of Huila (Colombia) is important. Dasypodoidea and Glyptodontoidea are represented respectively by Kraglievichia paranensis, Asterostemma cf. venezolensis and Propalaehoplophorus sp. These forms are distributed throughout the entire 700 m thick Honda group in La Venta. The morphology and size of the plates are individually variable characters related to their position in the carapace. The existence of a gradual variation in these characters creates difficulty in the separation of genus and species when dealing with isolated plates. The validity of some genera which were created on the basis of plates is questioned. It appears that excessive discrimination produced a plethora of forms and a review of these families is necessary.

DE - DESCRIPTORS: Cenozoic-; Chordata-; Colombia-; edentates-; La-Venta-area; Mammalia-; Miocene-; Neogene-; paleontology-; South-America; Tertiary-; Tetrapoda-; Vertebrata-

CC - CATEGORY CODES: 11-Vertebrate-paleontology

DT - DOCUMENT TYPE: Serial

BL - BIB LEVEL: Analytic

IL - ILLUSTRATION: illus.

RF - REFERENCE SOURCE: GeoRef, Copyright 2000, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States


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