Maria Antonieta Lorente

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Maria Antonieta Lorente is a geologist who specializes in stratigraphy and biostratigraphy. [1] [2]

Contents

Education

Maria Antonieta has attended two different universities to complete her education. During Maria's time at the University of Amsterdam, she received her Doctor in Mathematics and Natural sciences degree. Previously at the Central University of Venezuela, she earned a Geological Engineering degree as well as an MSc (Master of Science) in Sedimentary Geology degree. [3] Maria also has completed her education as a Technologist in the Food industry. [4]

Career

Maria Antonieta Lorente began her career as a lecturer in Historical Geology and Paleontology at the Central University of Venezuela. Maria excelled as a micropaleontologist adept in Palynology, developing a patent that used quantitative palynofacies for reservoir characterization and correlation. [1] Lorente started working as palynologists in Maraven SA. Later as a career specialist, she led a multidisciplinary team of sedimentologists, geochemists, petrophysics, and biostratigraphers. Her team supported the exploratory activities of the company. Eventually, Lorente became Head of Geological Laboratories as well as Leader of Stratigraphy; gaining the responsibility of leadership for teams of experts. Lorente also continued to manage these experts' team during this time overseeing specialized geological information. [1] She was then promoted to the role of "Planning and Strategy Manager" at PDVSA where she proposed the 2001 plan for the Exploration Business Unit's short, medium, and long-term objectives. [3] Maria Antonieta Lorente eventually retired from PDVSA with the aspirations of creating her own consulting service in the field of geology and environmental sciences. Years later her career path shifted shortly to the food industry where she had success with research and development, along with environmental efforts for a local company in Spain. [1] Lorente currently teaches online and mentors younger generations of Geology students at the Central University of Venezuela while also working as an International Consultant in Geology. [1] She is also currently a senior advisor to Ellington Geological Services in Houston Texas. [5]

Notable achievements

Maria Antonieta Lorente was awarded the AAPG Distinguished Service award in 1996. This award is "presented to members who have distinguished themselves in singular and beneficial long-term service to AAPG". [6]

Maria Antonieta Lorente was chosen as one of the nine convenors for the Paleogeography and Hydrocarbon Potential of the La Luna Formation and Related Cretaceous Anoxic Depositional Systems for the September 7–9 meeting in 2000. This meeting took place in Caracas, Venezuela. [7]

Publications

Maria Antioneta Lorente has published over 60 articles in geology, stratigraphy and petroleum geology.

Related Research Articles

<span class="mw-page-title-main">Zulia</span> State in Venezuela

Zulia State is one of the 23 states of Venezuela. The state capital is Maracaibo. As of the 2011 census, it has a population of 3,704,404, the largest population among Venezuela's states. It is also one of the few states in Venezuela in which voseo is widespread. The state is coterminous with the eponymous region of Zulia.

<span class="mw-page-title-main">Maracaibo Basin</span> Foreland basin in Venezuela

The Maracaibo Basin, also known as Lake Maracaibo natural region, Lake Maracaibo depression or Lake Maracaibo Lowlands, is a foreland basin and one of the eight natural regions of Venezuela, found in the northwestern corner of Venezuela in South America. Covering over 36,657 square km, it is a hydrocarbon-rich region that has produced over 30 billion bbl of oil with an estimated 44 billion bbl yet to be recovered. The basin is characterized by a large shallow tidal estuary, Lake Maracaibo, located near its center. The Maracaibo basin has a complex tectonic history that dates back to the Jurassic period with multiple evolution stages. Despite its complexity, these major tectonic stages are well preserved within its stratigraphy. This makes The Maracaibo basin one of the most valuable basins for reconstructing South America's early tectonic history.

<span class="mw-page-title-main">Urbión Group</span>

The Urbión Group is a geological group in Castile and León and La Rioja, Spain whose strata date back to the Early Cretaceous (late Hauterivian to late Barremian. The formations of the group comprise a sequence of brown limestones in a matrix of black silt, sandstones, claystones and conglomerates deposited under terrestrial conditions, in alluvial fan and fluvial environments.

The Tera Group is a geological group in the Cameros Basin and Sierra de la Demanda in Burgos, Spain. The group contains several formations whose strata date back to the Early Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.

<span class="mw-page-title-main">Camarillas Formation</span> Geological formation in Teruel and La Rioja, Spain

The Camarillas Formation is a geological formation in the Teruel Province of Aragón, Spain whose strata date back to the Early Cretaceous. The sandstones, mudstones and conglomerates of the formation, that due to syn-sedimentary faulting varies greatly in thickness from 300 to 800 metres, were deposited in fluvial, deltaic and lacustrine environments.

<span class="mw-page-title-main">Enciso Group</span>

The Enciso Group is a geological formation in La Rioja, Spain whose strata date back to the Early Cretaceous.

The South American land mammal ages (SALMA) establish a geologic timescale for prehistoric South American fauna beginning 64.5 Ma during the Paleocene and continuing through to the Late Pleistocene. These periods are referred to as ages, stages, or intervals and were established using geographic place names where fossil materials where obtained.

<span class="mw-page-title-main">Itaboraian</span>

The Itaboraian age is a period within the Early Eocene geologic time epoch of the Paleogene, used more specifically with South American land mammal ages (SALMA). It follows the Riochican and precedes the Casamayoran age.

The Riochican age is a period of geologic time within the Paleocene and Eocene epochs of the Paleogene, used more specifically within the South American land mammal ages (SALMA). It follows the Peligran and precedes the Itaboraian age.

<span class="mw-page-title-main">Neuquén Basin</span> Sedimentary basin covering most of Neuquén Province in Argentina

Neuquén Basin is a sedimentary basin covering most of Neuquén Province in Argentina. The basin originated in the Jurassic and developed through alternating continental and marine conditions well into the Tertiary. The basin bounds to the west with the Andean Volcanic Belt, to the southeast with the North Patagonian Massif and to the northeast with the San Rafael Block and to the east with the Sierra Pintada System. The basin covers an area of approximately 120,000 square kilometres (46,000 sq mi). One age of the SALMA classification, the Colloncuran, is defined in the basin, based on the Collón Curá Formation, named after the Collón Curá River, a tributary of the Limay River.

The Cerro Fortaleza Formation, in older literature described as Pari Aike Formation, is a Late Cretaceous geologic formation of Campanian to Maastrichtian age of the Austral Basin in southern Patagonia, Argentina.

<span class="mw-page-title-main">Malargüe Group</span>

The Malargüe Group is a group of geologic formations of the Neuquén Basin of the Mendoza, Neuquén, Río Negro and La Pampa Provinces in northern Patagonia, Argentina. The formations of the Malargüe Group range in age between the middle Campanian to Deseadan, an Oligocene age of the SALMA classification, straddling the Cretaceous–Paleogene boundary, about 79 million to 30 million years in age. The group overlies the older Neuquén Group, separated by an unconformity dated to 79 Ma. The rocks of the Malargüe Group comprise both marine and continental deposits which are over 400 m (1312 ft) thick in total.

<span class="mw-page-title-main">Middle Magdalena Valley</span>

The Middle Magdalena Valley, Middle Magdalena Basin or Middle Magdalena Valley Basin is an intermontane basin, located in north-central Colombia between the Central and Eastern Ranges of the Andes. The basin, covering an area of 34,000 square kilometres (13,000 sq mi), is situated in the departments of Santander, Boyacá, Cundinamarca and Tolima.

<span class="mw-page-title-main">Golfo San Jorge Basin</span>

The Golfo San Jorge Basin is a hydrocarbon-rich sedimentary basin located in eastern Patagonia, Argentina. The basin covers the entire San Jorge Gulf and an inland area west of it, having one half located in Santa Cruz Province and the other in Chubut Province. The northern boundary of the basin is the North Patagonian Massif while the Deseado Massif forms the southern boundary of the basin. The basin has largely developed under condition of extensional tectonics, including rifting.

Salta Basin or Salta Rift Basin is a sedimentary basin located in the Argentine Northwest. The basin started to accumulate sediments in the Early Cretaceous (Neocomian) and at present it has sedimentary deposits reaching thicknesses of 5,000 metres (16,000 ft). The basin contains seven sub-basins: Tres Cruces, Lomas de Olmedo, Metán, Alemanía, Salfity, El Rey, Sey and Brealito. The basin environment has variously been described as a "foreland rift" and an "intra-continental rift". The basin developed under conditions of extensional tectonics and rift-associated volcanism.

<span class="mw-page-title-main">Cesar-Ranchería Basin</span> Geologic formation in Colombia

The Cesar-Ranchería Basin is a sedimentary basin in northeastern Colombia. It is located in the southern part of the department of La Guajira and northeastern portion of Cesar. The basin is bound by the Oca Fault in the northeast and the Bucaramanga-Santa Marta Fault in the west. The mountain ranges Sierra Nevada de Santa Marta and the Serranía del Perijá enclose the narrow triangular intermontane basin, that covers an area of 11,668 square kilometres (4,505 sq mi). The Cesar and Ranchería Rivers flow through the basin, bearing their names.

<span class="mw-page-title-main">Bolivar Coastal Fields</span>

The Bolivar Coastal Fields (BCF), also known as the Bolivar Coastal Complex, is located on the eastern margin of Lake Maracaibo, Venezuela. Bolivar Coastal Field is the largest oil field in South America with its 6,000-7,000 wells and forest of related derricks, stretches thirty-five miles along the north-east coast of Lake Maracaibo. They form the largest oil field outside of the Middle East and contain mostly heavy oil with a gravity less than 22 degrees API. Also known as the Eastern Coast Fields, Bolivar Coastal Oil Field consists of Tía Juana, Lagunillas, Bachaquero, Ceuta, Motatán, Barua and Ambrosio. The Bolivar Coast field lies in the Maracaibo dry forests ecoregion, which has been severely damaged by farming and ranching as well as oil exploitation. The oil field still plays an important role in production from the nation with approximately 2.6 million barrels of oil a day. It is important to note that the oil and gas industry refers to the Bolivar Coastal Complex as a single oilfield, in spite of the fact that the oilfield consists of many sub-fields as stated above.

The geology of Venezuela includes ancient Precambrian igneous and metamorphic basement rocks, layered with sedimentary rocks from the Paleozoic and Mesozoic and thick geologically recent Cenozoic sediments with extensive oil and gas.

<span class="mw-page-title-main">Agrio Formation</span>

The Agrio Formation is an Early Cretaceous geologic formation that is up to 1,500 metres (4,900 ft) thick and is located in the southern Mendoza Province and northern-central Neuquén Province, in the Neuquén Basin of northwestern Patagonia, Argentina. This formation is the youngest one of the Mendoza Group, overlying the Mulichinco and Bajada Colorada Formations and overlain by the Huitrín and La Amarga Formations. It is dated to the Late Valanginian to Early Hauterivian, Late Valanginian to Early Barremian, or Hauterivian to earliest Aptian.

References

  1. 1 2 3 4 5 "Maria Antonieta Lorente: About me". Maria Antonieta Lorente. Retrieved 2021-04-12.
  2. ↑ "Dr Maria Antonieta Lorente - ALS Global" (PDF). Retrieved 2021-04-12.{{cite web}}: CS1 maint: url-status (link)
  3. 1 2 "News & Events-Ellington and Associates, Inc". www.ellingtongeologic.com. Retrieved 2021-04-22.
  4. ↑ "Resume Geology". Lorente María Antonieta. 2012-10-14. Retrieved 2021-04-22.
  5. ↑ "Maria Antonieta Lorente". ResearchGate. Retrieved 2021-04-22.{{cite web}}: CS1 maint: url-status (link)
  6. ↑ "Distinguished Service Award". www.aapg.org. Retrieved 2021-04-12.
  7. ↑ "Society for Sedimentary Geology". www.sepm.org. Retrieved 2021-04-22.{{cite web}}: CS1 maint: url-status (link)
  8. ↑ Lorente, María Antonieta (January 1977). "Paleoambiente del Miembro Quevedo (Formación Navay) en las proximidades de Santa Bárbara". Actas 5o. Congreso Geológico Venezolano.
  9. ↑ Lorente, Maria A. (1986-12-22). "Palynology and palynofacies of the upper tertiary in Venezuela". www.schweizerbart.de. Retrieved 2021-04-18.
  10. ↑ Azpiritxaga, I.; Lorente (1988). "Sand depositional styles in lower Lagunillas member (Lower Miocene) of Central-Western area of Maracaibo Lake, Venezuela, and their influence in reservoir modeling". doi:10.1306/703C829F-1707-11D7-8645000102C1865D. S2CID   140603013.{{cite journal}}: Cite journal requires |journal= (help)
  11. ↑ Boesi, T.; Galea, F.; Rojas, G.; Lorente, M. A.; Durán, I.; Velasquez, M. (1988). "Estudio Estratigrafico del Flanco Norandino en el Sector Lobatera-El Vigia [PAPER IN SPANISH] Stratigraphic Study of the North Andean Flank Region in Lobatera-El Vigia".{{cite journal}}: Cite journal requires |journal= (help)
  12. ↑ Boesi, T.; Galea, F.; Rojas, G.; Lorente, M. A.; Duran, I.; Velasquez, M. (1988-03-13). "Estudio Estratigrafico del Flanco Norandino". 3rd Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers. pp. cp. doi:10.3997/2214-4609-pdb.114.001.
  13. ↑ Battin, Tom J. (June 1998). "Dissolved organic matter and its optical properties in a blackwater tributary of the upper Orinoco river, Venezuela". Organic Geochemistry. 28 (9–10): 561–569. Bibcode:1998OrGeo..28..561B. doi:10.1016/s0146-6380(98)00028-x. ISSN   0146-6380.
  14. ↑ Lorente, M. A. (1990). "Digital image analysis : An approach for quantitative characterisation of organic facies and palynofacies". 45: 103–109.{{cite journal}}: Cite journal requires |journal= (help)
  15. ↑ US 4918739,Lorente, Maria A.; De Rincon, Jeanny T.& Morean, Orlandoet al.,"Process and system for digital analysis of images applied to stratigraphic data",published 1990-04-17, assigned to Maraven S.A.
  16. ↑ Lorente, María Antonieta (November 1990). "A multilevel approach to organic matter classification by Lorente M.A. & P. van Bergen". Stuifmail. Paleobotanical and Palynological Society of Utrecht.
  17. ↑ Boesi, H. T. R.; Lorente, M. A.; Mompart, L.; Murat, B.; Testamarck; Facon, R. (1993-02-01). "Facies and sedimentary environments of the cretaceous La Luna Formation in San Pedro Del Rio section, Venezuelan Andes: A multidisciplinary study". AAPG Bulletin (American Association of Petroleum Geologists); (United States). 77:2. ISSN   0149-1423. OSTI   6064898.
  18. ↑ Lorente, María Antonieta (1995). "EL PALEOGENO EN LA CUENCA DE MARACAIBO, VENEZUELA". Publicación Electrónica de la Asociación Paleontológica Argentina (in Spanish). 3 (1). ISSN   2469-0228.
  19. ↑ Hoorn, Carina; Guerrero, Javier; Sarmiento, Gustavo A.; Lorente, Maria A. (1995-03-01). "Andean tectonics as a cause for changing drainage patterns in Miocene northern South America". Geology. 23 (3): 237–240. Bibcode:1995Geo....23..237H. doi:10.1130/0091-7613(1995)023<0237:ATAACF>2.3.CO;2. ISSN   0091-7613.
  20. ↑ Lorente, María Antonieta (January 1995). "Late Cretaceous in Western Venezuela: a review and new biostratigraphical data (Extended Abstract)". IGCP 362 Annual Meeting, Maastricht.
  21. ↑ Olivares, C.; Lorente, M. A.; Cassani, F. (1996-08-01). "Geochemistry and organic facies of La Luna-Tres Esquinas cycle: Maturity, biomarkers and kerogen issues". AAPG Bulletin. 80 (8). OSTI   421157.
  22. ↑ Lorente, María Antonieta (January 1997). "Nuevos aportes para la datación de los principales eventos tectónicos y unidades litoestratigráficas de la cuenca de Maracaibo". Dirección General Sectorial.
  23. ↑ Erlich, R. N.; Pocknall, D. T.; Yeilding, C. A.; Lorente, M. Antonieta (1997-12-01). "Chronostratigraphy, Depositional Environments, and Reservoir Potential of Eocene Rocks, Southern and Central Merida Andes (Maracaibo and Barinas/Apure Basins), Western Venezuela". Shallow Marine and Nonmarine Reservoirs: Sequence Stratigraphy, Reservoir Architecture and Production Characteristics. doi:10.5724/gcs.97.18.0093. ISBN   978-1-944966-31-7.
  24. ↑ Pocknall, D. T.; Erlich, R. N.; Stein, J. A.; Bergen, J. A.; Lorente, M. Antonieta (1997). "A Cretaceous-Tertiary Boundary Section at Rio Lora, Merida Andes, Western Venezuela".{{cite journal}}: Cite journal requires |journal= (help)
  25. ↑ Pestman, Pieter; Ghosh, Santosh; Melendez, Luis; Lorente, Maria Antonieta (1997). "Marco Tectonoestratigráfico y Paleogeografía de la Cuenca de Maracaibo durante el Paleógeno [PAPER IN SPANISH] Tectonostratigraphic Framework and Paleogeography of the Maracaibo Basin during the Paleogene".{{cite journal}}: Cite journal requires |journal= (help)
  26. ↑ Erlich, R. N.; Nederbragt, A. J.; Lorente, M. Antonieta (1997). "Origin and Depositional Environments of Turonian – Maastrichtian Organic-Rich and Phosphatic Sediments of Western Venezuela".{{cite journal}}: Cite journal requires |journal= (help)
  27. ↑ Rull, Valentí; Lorente, Maria (1997-01-01). "Area central del Lago de Maracaibo: la bioestratigrafía como herramienta para la interpretación paleoestructural del Eoceno".{{cite journal}}: Cite journal requires |journal= (help)
  28. ↑ Lorente, María Antonieta. "Nuevas determinaciones de carbono orgánico total (COT) en formaciones cretácicas con perfiles convencionales en el noroeste del Lago de Maracaibo, Estado Zulia".{{cite journal}}: Cite journal requires |journal= (help)
  29. ↑ "Abstract: Estudio Sedimentologico de la Formacion Misoa en la Serrania de Trujillo, Estado Zulia, by F. Marquez, G. Bertorelli, E. Zapata, R. Falcsn, V. Padrsn, and O. Rey; #90951 (1996)". www.searchanddiscovery.com. Retrieved 2021-04-20.
  30. ↑ Pestman, P.; Ghosh, S.; Melendez, L.; Lorente, M. A. (1997-09-14). "Macro Estructural y Paleogeografia de la Cuenca de Maracaibo durante el Paleógeno". 6th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers. pp. cp. doi:10.3997/2214-4609-pdb.117.084esp.
  31. ↑ Lorente, María Antonieta (January 1997). "Implicaciones Tectónicas de un Evento Estructural en el Cretácico Superior (Santoniense - Campaniense) de Venezuela Occidental". Memorias: VIII Congreso Geologico Venezolano.
  32. ↑ Erlich, R.N; MacSotay i, O.; Nederbragt, A.J; Lorente, M.Antonieta (1999-09-15). "Palaeoecology, palaeogeography and depositional environments of Upper Cretaceous rocks of western Venezuela". Palaeogeography, Palaeoclimatology, Palaeoecology. 153 (1–4): 203–238. Bibcode:1999PPP...153..203E. doi:10.1016/S0031-0182(99)00072-3. ISSN   0031-0182.
  33. ↑ Erlich, R.N; Palmer-Koleman, S.E; Lorente, M.Antonieta (1999-10-01). "Geochemical characterization of oceanographic and climatic changes recorded in upper Albian to lower Maastrichtian strata, western Venezuela". Cretaceous Research. 20 (5): 547–581. Bibcode:1999CrRes..20..547E. doi:10.1006/cres.1999.0167. ISSN   0195-6671.
  34. ↑ "Late Cretaceous Anoxia and Lateral Microfacies Changes in the Tres Esquinas Member, La Luna Formation, Western Venezuela". ResearchGate. Retrieved 2021-04-20.
  35. ↑ Lorente, María Antonieta. "Diagenetic Evaluation of La Luna Formation at Tachira and Merida States, Western Venezuela".{{cite journal}}: Cite journal requires |journal= (help)
  36. ↑ Lorente, María Antonieta. "Late Cretaceous Upwelling in the Southwest of the Thetys Sea, a Case History From the Barinas Basin, Venezuela. Extended Abtract".{{cite journal}}: Cite journal requires |journal= (help)
  37. 1 2 Lane, Richard H.; Steininger, Fritz F.; Kaesler, Roger L.; Ziegler, Willi; Lipps, Jere (2000-01-01). "Fossils and the future". www.schweizerbart.de. Retrieved 2021-04-18.
  38. ↑ Erlich, R.N.; MacSotay i, O.; Nederbragt, A.J.; Antonieta Lorente, M. (2000-05-01). "Birth and death of the Late Cretaceous "La Luna Sea", and origin of the Tres Esquinas phosphorites". Journal of South American Earth Sciences. 13 (1–2): 21–45. Bibcode:2000JSAES..13...21E. doi:10.1016/S0895-9811(00)00016-X. ISSN   0895-9811.
  39. ↑ "ABSTRACT: Seismostratigraphic Study of a Miocene-Pleistocene Subsurface Interval, Northern Monagas, Eastern Venezuela Basin, by Lorena G. Moscardelli J. and María Antonieta Lorente; #90906(2001)". www.searchanddiscovery.com. Retrieved 2021-04-20.
  40. ↑ David T. Pocknall, Robert N. Erlcih, Jeffrey A. Stein, Maria A. Lorente (2001). "The palynofloral succession across the Cretaceous to Paleocene transition zone, Merida Andes, Western Venezuela". 9th International Palynological Congress. Proceedings of the 9th International Palynological Congress – via ResearchGate.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  41. ↑ Gonzalez, E.; Lorente, M.; Acosta, J.; Rull, V. (2001-07-01). "Series analysis application of time for cyclic pattern determination in the Cretaceous-Tertiary limit (Venezuela western); Aplicacion de analisis de series de tiempo para la determinacion de la ciclicidad en el limite cretacico-terciario (oeste de Venezuela)" (in Spanish).{{cite journal}}: Cite journal requires |journal= (help)
  42. ↑ Lorente, María Antonieta (January 2003). "Cicloestratigrafía de las Formaciones Morichito, Las Piedras y Mesa, Norte de Monagas, Venezuela Oriental". I Er Congreso Virtual de Sedimentologia, Caracas, Venezuela.
  43. ↑ "Biofacies development related to upwelling systems based on high-resolution biostratigraphic studies in southwest Venezuela | Request PDF". ResearchGate. Retrieved 2021-04-20.
  44. ↑ "View PDF". www.searchanddiscovery.com. Retrieved 2021-04-20.
  45. ↑ "View PDF". www.searchanddiscovery.com. Retrieved 2021-04-20.
  46. ↑ Zapata, Eglee; Padron, Victor; Madrid, Isiris; Kertznus, Vanessa; Truskowski, Irene; Lorente, Maria Antonieta (2003-10-01). "Biostratigraphic, Sedimentologic, and Chemostratigraphic Study of the La Luna Formation (Late Turonian–Campanian) in the San Miguel and Las Hernández Sections, Western Venezuela". PALAIOS. 18 (4–5): 367–377. Bibcode:2003Palai..18..367Z. doi:10.1669/0883-1351(2003)018<0367:BSACSO>2.0.CO;2. ISSN   0883-1351. S2CID   129586117.
  47. ↑ Bralower, Timothy J.; Lorente, Maria Antonieta (2003-10-01). "Paleogeography and Stratigraphy of the La Luna Formation and Related Cretaceous Anoxic Depositional Systems". PALAIOS. 18 (4–5): 301–304. Bibcode:2003Palai..18..301B. doi:10.1669/0883-1351(2003)018<0301:PASOTL>2.0.CO;2. ISSN   0883-1351. S2CID   130701978.
  48. ↑ Parra, Marien; Moscardelli, Lorena; Lorente, Maria Antonieta (2003-10-01). "Late Cretaceous Anoxia and Lateral Microfacies Changes in the Tres Esquinas Member, La Luna Formation, Western Venezuela". PALAIOS. 18 (4–5): 321–333. Bibcode:2003Palai..18..321P. doi:10.1669/0883-1351(2003)018<0321:LCAALM>2.0.CO;2. ISSN   0883-1351. S2CID   131470871.
  49. ↑ Rey, O.; Simo (Toni), J.A; Lorente, M.A (2004-08-02). "A record of long- and short-term environmental and climatic change during OAE3: La Luna Formation, Late Cretaceous (Santonian–early Campanian), Venezuela". Sedimentary Geology. 170 (1–2): 85–105. Bibcode:2004SedG..170...85R. doi:10.1016/j.sedgeo.2004.06.006. ISSN   0037-0738.
  50. ↑ Cooney, P. M.; Lorente, M. A. (2009-01-01). "A structuring event of Campanian age in western Venezuela, interpreted from seismic and palaeontological data". Geological Society, London, Special Publications. 328 (1): 687–703. Bibcode:2009GSLSP.328..687C. doi:10.1144/SP328.27. ISSN   0305-8719. S2CID   129720105.
  51. ↑ James, K. H.; Lorente, M. A.; Pindell, J. L. (2009-01-01). "The Origin and Evolution of the Caribbean Plate". Geological Society, London, Special Publications. 328 (1). doi:10.1144/SP328.
  52. ↑ Salazar, Migdalys; Moscardelli, Lorena; Fisher, William; Lorente, Maria Antonieta (2011-01-01). "Tectonostratigraphic evolution of the Morichito piggyback basin, Eastern Venezuelan Basin". Marine and Petroleum Geology. 28 (1): 109–125. Bibcode:2011MarPG..28..109S. doi:10.1016/j.marpetgeo.2009.07.004. ISSN   0264-8172.
  53. ↑ "AAPG Top 100 Papers". 100years.aapg.org. Retrieved 2021-04-20.
  54. ↑ Kariminia, S. Mohsen; Pletka, Crystal; Elderbak, Khalifa; Liu, Xiuju; Xiong, Chan; Vodo, Themi; Hojnacki, Paul; Porter, Benjamin; Greene, James; Lorente, Maria A. "Geochemical and Foraminiferal Responses to Anthropogenic Activities Along the Coastal Regions of Matagorda and Brazoria Counties, Texas".{{cite journal}}: Cite journal requires |journal= (help)
  55. ↑ Russo1, Fabio; Brown1, Christopher; Hinote1, Russell; Hodson2, James; Kariminia1, Mohsen; Lorente1, Maria; Wells1, Christopher. "A Multidisciplinary Study on a Representative Section From Masirah Basin-Oman".{{cite journal}}: Cite journal requires |journal= (help)
  56. ↑ Liu, Xiuju; Xiong, Yingqian; Vodo, Themi; Smith, Alan; Lorente, Maria Antonieta. "Advanced Quantitative Stratigraphic Data Integration of Conventional and Unconventional Plays".{{cite journal}}: Cite journal requires |journal= (help)
  57. ↑ Capello, Maria Angela; Lorente, Maria Antonieta; Serrano, Isabel; Flores, Monica; Briceno, Maria Gabriela (2020-10-19). "The Evolution of Women's Role in Engineering and Geosciences in the Oil Industry From the 20th to the 21st Century: A Documented Case History From Venezuela". Day 3 Wed, October 28, 2020. OnePetro. doi:10.2118/201359-MS. S2CID   226324413.
  58. ↑ Lorente, M. A. (2021-03-09). "Palynofacies, environments, and climate changes in the Magdalena River Basin". bioRxiv: 2021.03.07.434303. doi:10.1101/2021.03.07.434303. S2CID   232224401.
  59. ↑ Lorente, Maria (2021-03-10). FIRST RESULTS FROM A QUANTITATIVE PALYNOFACIES STUDY OF RECENT ENVIRONMENTS FROM THE LOWER MAGDALENA RIVER BASIN, COLOMBIA.
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