Relevant bibliographies by topics / Guajira Basin

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers

Academic literature on the topic 'Guajira Basin'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Guajira Basin"

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Eissa, Mohamed A., John Pfeiffer, and Heiman Alfredo Paz Ortega. "Seismic petrophysical analysis for thin sandstone reservoirs in Colombia's Guajira Basin." Leading Edge 28, no. 6 (June 2009): 640–47. http://dx.doi.org/10.1190/1.3148402.

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Londoño-Burbano, Alejandro, César Román-Valencia, and Donald C. Taphorn. "Taxonomic review of Colombian Parodon (Characiformes: Parodontidae), with descriptions of three new species." Neotropical Ichthyology 9, no. 4 (2011): 709–30. http://dx.doi.org/10.1590/s1679-62252011000400003.

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We review species of Parodon Valenciennes, 1850 from the Magdalena, Cauca, Orinoco, Amazonas, Atrato and Caribbean-Guajira River basins of Colombia using meristic and morphological characters. We recognize eight valid species, five previously described: P. apolinari Myers, from the Orinoco River basin; P. buckleyi Boulenger and P. pongoensis (Allen) from the upper Amazon; P. caliensis Boulenger, from the upper Cauca River drainage; and P. suborbitalis Valenciennes, from Lake Maracaibo basin. Three new species are described: P. alfonsoi, from the lower Magdalena River drainage; P. magdalenensis, from the middle Magdalena and upper Cauca River drainages; and P. atratoensis, from the Atrato River basin. We redescribe Parodon suborbitalis using type specimens and topotypes, and designate lectotypes. A taxonomic key is included for identification of the species, as well as geographic distribution maps.
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Moreno, F., A. J. W. Hendy, L. Quiroz, N. Hoyos, D. S. Jones, V. Zapata, S. Zapata, et al. "Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia." Swiss Journal of Palaeontology 134, no. 1 (April 4, 2015): 5–43. http://dx.doi.org/10.1007/s13358-015-0071-4.

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Silva-Tamayo, Juan Carlos, Catalina Ramirez, Mario Lara, Alcides Nobrega Sial, David Trujillo, and Edward Salazar. "Sedimentology and chemostratigraphy of a Valanginian carbonate succession from the Baja Guajira Basin, northern Colombia." Brazilian Journal of Geology 46, suppl 1 (June 2016): 163–80. http://dx.doi.org/10.1590/2317-488920160030294.

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ABSTRACT: The Kesima Member of the Palanz Formation constitutes the first record of Cretaceous marine sedimentation along the Baja Guajira Basin, northern Colombia. Sedimentologic and petrographic analyses suggest a deposition along a coral reef dominated rimmed carbonate platform. 87Sr/86Sr values between 0.707350 and 0.707400 suggest a Valanginian (136 - 132 Ma) depositional age for the Kesima Member. A positive anomaly on the δ13C values of ~2.2‰ suggests that this rimmed carbonate platform registered the Valanginian Weissert oceanic anoxic event. Although the Weissert oceanic anoxic event resulted on a major drowning of the Circum Tethyan carbonate platforms, it seems to have not affected those from the Circum Caribbean, where several shallow marine carbonate platform successions crop out. The Kesima Member displays a change from an organically produced carbonate factory into an inorganically produced, ooids dominated, carbonate factory during the peak of the Weissert event δ13C anomaly. This change in the carbonate factory, which may represent a major perturbation of the marine carbonate budget along tropical settings during the Weissert event, coincides with a major decrease in global sea level. Finally, the age of the Kesima Member is considerably older than that of other Cretaceous carbonate successions cropping out in other northern South America sedimentary basins (i.e. Perija-Merida, Cesar-Rancheria). Differences in the timing of the Cretaceous marine incursion along northern South America, together with the differences in the Triassic-Jurassic stratigraphy of several sedimentary basins in northern South America, suggest that the Baja Guajira and Maracaibo basins remained as an isolated tectonic block separated from northern South America after the breakup of Pangea.
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Flórez, Paola, Paula Zapata-Ramírez, and James S. Klaus. "Early Miocene shallow-water corals from La Guajira, Colombia: part I, Acroporidae–Montastraeidae." Journal of Paleontology 93, no. 1 (October 2, 2018): 1–24. http://dx.doi.org/10.1017/jpa.2018.45.

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AbstractWe document for the first time Miocene corals from the Siamaná and Jimol formations of the Cocinetas Basin in La Guajira Peninsula, northern Colombia. This is the first of two contributions dedicated to the description and detailed illustration of morphospecies collected during two scientific expeditions (2011, 2014) to the remote region. Here we report coral morphospecies attributed to the families Acroporidae, Agathiphylliidae, Astrocoeniidae, Caryophylliidae, Diploastraeidae, Merulinidae, and Montastraeidae. Eighteen species belonging to these seven families, included in nine genera, are described. Fifteen species are assigned to established taxa, while three remain in open nomenclature. Of the species identified, onlyMontastraea cavernosa(Linnaeus, 1767) exists today. The coral taxa described are typical of the Oligocene–Miocene transition and were important components of shallow-water reefs in the Caribbean and Gulf of Mexico region during this period. The occurrence ofAgathiphylliaspp.,Antiguastrea, andDiploastreaspp. confirms the presence of these genera in the Miocene of the Southern Caribbean. Coral assemblages suggest that the La Guajira coral community thrived in calm and shallow waters.
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Rangel, A., B. Katz, V. Ramirez, and E. Vaz dos Santos Neto. "Alternative interpretations as to the origin of the hydrocarbons of the Guajira Basin, Colombia." Marine and Petroleum Geology 20, no. 2 (February 2003): 129–39. http://dx.doi.org/10.1016/s0264-8172(03)00061-8.

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Vence, Eleine, and Paul Mann. "Subsurface basement, structure, stratigraphy, and timing of regional tectonic events affecting the Guajira margin of northern Colombia." Interpretation 8, no. 4 (November 1, 2020): ST69—ST105. http://dx.doi.org/10.1190/int-2020-0016.1.

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We have combined previous data from Mesozoic-Cenozoic outcrops in the Guajira Peninsula of northern Colombia with regional gravity, bathymetric, and seismic interpretations to demonstrate the existence of a 280 km long western extension of the Great Arc of the Caribbean (GAC) along the continental margin of Colombia. Seismic data reveal an 80–100 km wide domal-shaped basement high that exhibits internal chaotic seismic facies. This elongate and domal-shaped structure extends 1800 km from the Aves Ridge in the Caribbean Sea to the study area in offshore Colombia. The western extension of the GAC in Colombia and western Venezuela is buried by 700–3000 m of continental margin sedimentary rocks as a result of the GAC colliding earlier with the Colombian margin (Cretaceous-early Paleogene collision) than its subaerially exposed eastern extension along the Leeward Antilles ridge (late Paleogene-Neogene). Our compilation of geologic information from the entire GAC reveals that GAC magmatism occurred from 128 to 74 Ma with magmatism ages progressively younger toward the east. Six upper Eocene to recent marine seismic sequences overlying the domal basement high of the GAC have been mapped by our analysis of 2400 km of seismic lines and 12 well logs. Based on subsurface mapping correlated with well-log information and onland geology in the Guajira Peninsula, these six sequences record four major deformational events: (1) late Eocene rifting in an east–west direction produced half-grabens in the northern part of the area, (2) Oligocene transtension in the southern part of the area expressed by right-lateral Oligocene strike-slip faulting and extensional basin formation, (3) early-middle Miocene transtension, and (4) late Miocene-early Pliocene Andean uplift accompanied by rapid erosion and clastic infilling of offshore basins by the Magdalena delta and deep-sea fan. The significance of this basin framework is discussed for known and inferred hydrocarbon systems.
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Carrillo-Briceño, Jorge Domingo, Zoneibe Luz, Austin Hendy, László Kocsis, Orangel Aguilera, and Torsten Vennemann. "Neogene Caribbean elasmobranchs: diversity, paleoecology and paleoenvironmental significance of the Cocinetas Basin assemblage (Guajira Peninsula, Colombia)." Biogeosciences 16, no. 1 (January 8, 2019): 33–56. http://dx.doi.org/10.5194/bg-16-33-2019.

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Abstract. The Cocinetas Basin is located on the eastern flank of the Guajira Peninsula, northern Colombia (southern Caribbean). During the late Oligocene through the Pliocene, much of the basin was submerged. The extensive deposits in this area suggest a transition from a shallow marine to a fluvio-deltaic system, with a rich record of invertebrate and vertebrate fauna. The elasmobranch assemblages of the early Miocene to the late Pliocene succession in the Cocinetas Basin (Jimol, Castilletes and Ware formations, as well as the Patsúa Valley) are described for the first time. The assemblages include at least 30 taxa of sharks (Squaliformes, Pristiophoriformes, Orectolobiformes, Lamniformes and Carcharhiniformes) and batoids (Rhinopristiformes and Myliobatiformes), of which 24 taxa are reported from the Colombian Neogene for the first time. Paleoecological interpretations are based on the feeding ecology and on estimates of the paleohydrology (relative salinity, temperature) using stable isotope compositions of oxygen in the bioapatite of shark teeth. The isotopic composition of the studied specimens corroborates paleoenvironmental settings for the studied units that were previously estimated based on the sedimentology and biology of the taxa. These Neogene elasmobranch assemblages from the Cocinetas Basin provide new insights into the diversity the sharks and rays inhabiting the coastal and estuarine environments of the northwestern margin of South America, both during the existence of the gateway between the Atlantic and Pacific oceans and following its closure.
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HRBEK, TOMAS, DONALD C. TAPHORN, and JAMIE E. THOMERSON. "Molecular phylogeny of Austrofundulus Myers (Cyprinodontiformes: Rivulidae), with revision of the genus and the description of four new species." Zootaxa 825, no. 1 (January 20, 2005): 1. http://dx.doi.org/10.11646/zootaxa.825.1.1.

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Phylogenetic analysis of 13 mitochondrial DNA genes of Austrofundulus Myers 1932 indicates that as presently recognized, A. limnaeus is composed of several populations with monophyletic haplotype lineages, which together are paraphyletic with respected to A. transilis. These populationswere previously united based on shared plesiomorphic morphometric characters. Austrofundulus myersi is removed from synonymy; four new species: A. rupununi, A. leohoignei, A. guajira, and A. leoni are described; and A. limnaeus is restricted to populations along the eastern side of Lake Maracaibo. In contrast, populations of A. transilis from the Río Apure Llanos and the lower Río Unare basin show little divergence. The proposed phylogeny: (A. myersi (A. leoni (A. limnaeus (A. guajira (A. leohoignei (A. rupununi (A. transilis))))))) is strongly supported by high bootstrap values and Bremer decay indexes, and unique length variations in the 12S ribosomal DNA (rDNA) gene. The distributions and the relationships of the newly erected species are concordant with the geological history of northern South America.Un análisis filogenético de 13 genes del ADN mitocondrial de Austrofundulus muestra que como actualmente este configurada, la especie Austrofundulus limnaeus es parafilética, y consiste de varias linajes monofiléticas que estuvieron unidas en base de características morfométricas plesiomórficas que comparten. Se remueve Austrofundulus myersi de la sinonímia de A. limnaeus, se describen cuatro especies nuevas: A. rupununi, A. leohoignei, A. guajira y A. leoni, y se restringe A. limnaeus a las poblaciones del lado este del Lago de Maracaibo. Muy distinta la situación de las diferentes poblaciones de A. transilis de las cuencas del Río Apure y Unare, que muestra poca divergencia genética. La filogenia propuesta es: (A. myersi (A. leoni (A. limnaeus (A. guajira (A. leohoignei (A. rupununi (A. transilis))))))) se apoya fuertemente por los altos valores bootstrap y los índices Bremer de descomposición y por variaciones únicas en la longitud del gen 12S de la ribosoma de RDN (rRDN). Las distribuciones zoogeográficas y las relaciones filogenéticas de las especies nuevas descritas concuerdan bien con la historia geológica del norte de Sudamérica.
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Jouanno, Julien, and Julio Sheinbaum. "Heat Balance and Eddies in the Caribbean Upwelling System." Journal of Physical Oceanography 43, no. 5 (May 1, 2013): 1004–14. http://dx.doi.org/10.1175/jpo-d-12-0140.1.

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Abstract The upper-ocean heat budget of the Caribbean upwelling system is investigated during the onset of the Atlantic warm pool (June–September) using high-resolution observations of sea surface temperature and a high-resolution (°) regional model. Vertical mixing is found to be the major cooling contribution to the mixed layer heat budget in the nearshore and offshore Colombia Basin. Numerical results show that intense mesoscale eddies in the Colombia Basin significantly shape the turbulent cooling and may participate in the maintenance of cooler temperature in this region compared to surrounding areas. Indeed, increased mixing at the base of the mixed layer occurs below energetic surface jets that form on the downstream side of the eddies. These jets generally flow offshore and may arise from the deformation of the surface mesoscale field. It is shown that significant contribution of horizontal advection to the mixed layer heat budget is limited to a radius of 300 km around the Guajira and Margarita upwelling zones.
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Dissertations / Theses on the topic "Guajira Basin"

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TARAZONA, DARWIN CLEMENTE MATEUS. "PORE PRESSURE ESTIMATION IN THE GUAJIRA BASIN, COLOMBIA, USING BASIN MODELING." PONTIFÍCIA UNIVERSIDADE CATÓLICA DO RIO DE JANEIRO, 2013. http://www.maxwell.vrac.puc-rio.br/Busca_etds.php?strSecao=resultado&nrSeq=23880@1.

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PONTIFÍCIA UNIVERSIDADE CATÓLICA DO RIO DE JANEIRO
COORDENAÇÃO DE APERFEIÇOAMENTO DO PESSOAL DE ENSINO SUPERIOR
PROGRAMA DE EXCELENCIA ACADEMICA
A caracterização das pressões de poros nas bacias sedimentares marinhas é fundamental dentro da etapa de planejamento dos projetos de perfuração na indústria do Petróleo. Uma vez que o desconhecimento dessas pressões coloca em risco a integridade das pessoas nas sondas de perfuração, o ambiente, além de causar grandes prejuízos para as companhias. As metodologias para a estimativa das poropressões na indústria do petróleo tiveram grande desenvolvimento a partir da década de1950. Porém, a grande maioria delas não levam em consideração caraterísticas geológicas importantes como a diagêneses das rochas, as condições de contorno para o fluxo de fluidos, e os mecanismos de dissipação das sobrepressões durante o tempo geológico. Por isso, o principal objetivo do trabalho é fortalecer os estudos convencionais de estimativa de pressão de poros incluindo uma metodologia não convencional com abordagem na modelagem de bacias. Essa metodologia permite analisar o fenômeno como um sistema dinâmico, bem como levar em consideração os mecanismos de geração e de dissipação das pressões durante a evolução geológica da Bacia. Apresenta-se a descrição dos principais mecanismos de geração de sobrepressão, a teoria que descreve o fenômeno das sobrepressões, as metodologias convencionais utilizadas na indústria do petróleo e as hipóteses da metodologia baseada na modelagem de bacias. Utilizou-se o software SEMIMT, do instituto de pesquisa da Noruega, o SINTEF, para realizar a estimativa das poropressões na Bacia de Guajira, uma região offshore do norte da Colômbia. A estimativa das pressões considerou os contornos da bacia, o modelo geológico da região, o histórico de soterramento da Bacia, bem como de modelos de compactação e os modelos de fluxo vertical e fluxo horizontal dos fluidos. O resultado da estimativa das pressões permitiu definir quatro zonas com diferente grau de sobrepressão na área em estudo, que foram comparados com uma metodologia convencional, bem com dados históricos de poços perfurados na região.
Pore pressure prediction is a critical issue for well planning in the oil and gas industry. It is even more critical for offshore environments due to high risks involved in drilling operation. Blowout is the main risk regarding pore pressure since it could cause rig explosion, and oil spills to environment. Such problems can lead a successful company to a very weak position. Therefore, since the fifties, several methodologies for pore pressure prediction have been developed for the industry. Most of them just consider the mechanism of compaction as the main cause of overpressure, ignoring other factors such as rock diagenesis, boundary conditions for fluid flow, and pressure dissipation during the geologic history. That is why the main objective of this work is improving current pore pressure studies, including an alternative methodology (developed by the Norway Petroleum Research Institute - SINTEF), from a scale of basin modeling. That methodology allows analyzing the pressure phenomenon like a dynamic system, where the interaction of the overpressure and the pressure dissipation mechanisms are considered during the geological history. In this paper, main characteristics of overpressure mechanisms are briefly described as well as common methodologies used in the Oil and Gas industry for pressure prediction. Furthermore, the most important hypothesis for basing modeling methodology is described. SEMIMT software was used to predict pore pressure in Guajira Basin, an offshore region located in north Colombia. Results of basin modeling methodology allowed defining four overpressure zones which fit adequately with wells data. Besides, that result was compared with a conventional methodology. Finally, a discussion about the results is presented, highlighting the main advantages and disadvantages observed in this research.
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Güiza, Helga Nayibe Niño. "Análise sismoestratigráfica do mioceno medio-inferior: oligoceno superior em uma área da guajira alta na Bacia Da Guajira, Colômbia." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2016. http://hdl.handle.net/10183/153270.

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O Caribe Colombiano é o foco da exploração na Colômbia, e a Bacia da Guajira na sua parte offshore tem sido relativamente pouco explorada. O presente trabalho tem como objetivo fazer um estudo sísmico de alta resolução aplicável á áreas sem exploração em blocos novos ou para ter diferentes perspectivas em blocos já explorados, neste caso para o intervalo de tempo compreendido entre o limite do Mioceno médio-inferior e o Oligoceno superior, em uma área da Guajira Alta. A partir da integração de duas seções sísmicas 2D, associadas a seis poços com litologias definidas por amostras de calha, foi realizada: (1) uma análise sismoestratigráfica de alta resolução incluindo a interpretação das terminações dos refletores, definição das unidades sismoestratigráficas e superfícies chave, (2) identificação das sismofácies, (3) a elaboração de uma carta cronoestratigráfica. Como resultado, foram individualizadas cinco unidades sísmicas, seis sismofácies e a carta cronoestratigráfica Todas as unidades sísmicas identificadas correspondem com depósitos de gravidade tipo fluxo de detritos e turbiditos, e depósitos hemipelágicos. As sismofácies caracterizadas como turbiditos (refletores paralelos, subparalelos, hummocky), são geralmente calcáreas, as sismofácies de fluxo de detritos (refletores caóticos), têm mistura de litologias tipo folhelhos, siltitos, lamitos, arenitos e carbonatos, e as sismofácies definidas como depósitos hemipelágicos (refletores paralelos, subparalelos), correspondem em sua maioria com depósitos finos. Na carta cronoestratigráfica indica uma depositacão contínua em esse intervalo de tempo.
Colombia Caribbean province is an important hydrocarbon exploration target in Colombia, a Guajira Offshore Basin as part of this province and is a frontier basin today. Main objective of this study is to develop a high resolution seismic stratigraphic study to be applied to unexplored areas on new blocks and/or to have another interpretation in low explored areas, in this case, on the specific time interval upper Oligocene-middle-lower Miocene, selecting a study area in Upper Guajira offshore. Data integration of two seismic sections and lithologic logs from six wells obtained from cuttings made possible to interpret: 1) High resolution seismic stratigraphic analysis including seismic stratigraphic units and key surfaces definition, seismic reflectors pinch outs, 2) seismic facies definition and 3) cronostratigraphic chart. From this analysis were stablished five seismic units, six seismic facies and a chronostratigraphic events chart. All interpreted seismic units correspond to gravity flow deposits debris and turbiditic type and hemipelagic deposits. Turbidite type seismic facies (parallel, subparallel and hummocky reflectors), are usually calcareous in composition, as well as detrital fluxes (chaotical reflectors), are generally a mixture of sandstones, limestones, siltstones, mudstones and shales, and hemipelagic seismic facies (parallel to subparallel reflectors) correspond to thin bedded deposits usually silty and muddy. Chronostratigraphic chart events indicates continuous deposition in this time interval.
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Wells, Shelley Lorraine. "Grave Matters: A Presentation and Comparative Analysis of the Late Classic Burials from Guajilar, Chiapas, Mexico." BYU ScholarsArchive, 2015. https://scholarsarchive.byu.edu/etd/8794.

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This thesis aims to identify the possible origins of the peoples who immigrated into the archaeological sites of Guajilar and Lagartero, located in the upper Grijalva River Basin region in southern Chiapas, Mexico, during the Late Classic period (AD 650-900). First, I present the Late Classic burial data from both sites according to four basic descriptive criteria: burial location, grave type, burial type, and grave goods. Then, I conduct a comparative analysis of the burial practices found at these two sites based on these criteria so that patterns in burial practices can be identified. Following the comparative analysis between Guajilar and Lagartero, I then compare their burial practices to those from two sites in the southern Maya Lowlands (Altar de Sacrificios and Seibal) and those found at various sites in the Guatemala Highlands (which border the upper Grijalva River Basin region to the north and east, respectively). The analysis reveals greater similarities in burial practices with sites in the Guatemala Highlands than with those in the southern Maya Lowlands. This suggests that peoples from the Guatemala Highlands were more likely to have immigrated into Guajilar and Lagartero during the Late Classic period.
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Book chapters on the topic "Guajira Basin"

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Katz, Barry, and Kenneth Williams. "Biogenic Gas Potential Offshore Guajira Peninsula, Colombia." In The Circum-Gulf of Mexico and the CaribbeanHydrocarbon Habitats, Basin Formation and Plate Tectonics. American Association of Petroleum Geologists, 2003. http://dx.doi.org/10.1306/m79877c43.

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Mitchell, Peter. "South America I: Caribbean Deserts and Tropical Savannahs." In Horse Nations. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780198703839.003.0012.

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These two quotations, dating to within almost a decade of each other, refer to very different parts of South America, the first the La Guajira Peninsula at its northern tip, the second the savannahs of the Gran Chaco at its very heart. The Wayúu, dwelling in the first, had no direct connection with the Mbayá of whom Dobrizhoffer wrote here (though he is more famous for his work on their cousins, the Abipones). Nevertheless, both regions shared aspects of their respective experiences of colonial intrusion and settlement: the frequent adoption not just of horses but also of other exotic species like cattle and sheep; Spanish use of missionaries to try and pacify their Indigenous inhabitants; and the fact that the latter could play off one European power, or Spanish province, against another, thereby maintaining their own freedom of action. Aiding the Native peoples in this was their geographically, politically, and economically marginal position with respect to the main foci of colonial power in the Andes and along the Atlantic. Spain began exploiting Venezuela’s pearl fisheries as early as 1508, even settling on the mainland from 1522, but the real impetus to conquest in South America came only with Francisco Pizarro’s invasion of the Inka Empire in 1533. The highlands of Peru, Bolivia, Ecuador, and Colombia (the latter never part of Inka domains), the lowlands between them and the Pacific Ocean, the northern half of Chile, and the northwestern corner of Argentina all passed quickly—if not always easily—under Spanish control. So too did parts of Paraguay, settled by following rivers inland from the Atlantic. Portugal, on the other hand, secured for herself the coast of Brazil, eventually expanding her reach across virtually the entire Amazon Basin. Horses were as much a part of the conquistadores’ repertoire in South America as in Mexico. They sowed panic when Pizarro first confronted Inka troops at Cajamarca in 1533, but Native American surprise and fear did not last. Inka armies quickly devised tactics to neutralize the effects of horses on the battlefield in vain efforts to expel the invader.
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Habtemariam, Solomon. "The chemical and pharmacological basis of guava (Psidium guajava L.) as potential therapy for type 2 diabetes and associated diseases." In Medicinal Foods as Potential Therapies for Type-2 Diabetes and Associated Diseases, 251–305. Elsevier, 2019. http://dx.doi.org/10.1016/b978-0-08-102922-0.00009-2.

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Conference papers on the topic "Guajira Basin"

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Escalante, C. E. "Seismic Stratigraphic of the Tayrona Depression-Offshore Baja Guajira Basin, Colombia." In 9th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609-pdb.111.142.

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Ramirez, V., A. Rangel, and R. Hernandez. "Thermogenic Hydrocarbon Processes In The Guajira Basin- A Petroleum Systems Approach." In 8th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.33.paper30.

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Olaya, I., and V. Ramírez. "Exploración En La Cuenca Frontera Guajira Costa-Afuera: Nuevos Conceptos Y Plays (New Play Concepts In The Offshore Guajira Frontier Basin)." In 8th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.33.paper86.

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CASTAÑEDA, CLAUDIA L. LONDOÑO, MIGUEL ANGEL DIAZ, YOMAIRA DEVIA, JUAN SEBASTIAN BALLEN, and JUAN DAVID BARRIOS. "MULTIFUNCTIONAL LANDSCAPES AND SOCIOECONOMIC IMPACTS: A CASE STUDY ON PRODUCTIVE SECTORS OF RANCHERÍA RIVER BASIN, GUAJIRA, COLOMBIA." In ENVIRONMENTAL IMPACT 2018. Southampton UK: WIT Press, 2018. http://dx.doi.org/10.2495/eid180271.

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Reeve, Andrew S., Efrén David Gómez Arévalo, and Ryan P. Gordon. "CREATING PLAUSIBLE GROUNDWATER FLOW MODELS FOR THE CARRAIPIA BASIN, LA GUAJIRA DEPARTMENT (COLOMBIA) TO AID IN WATER RESOURCE MANAGEMENT." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-339068.

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