AB STRA CT Th e Cam pos Basin is located offshore the State of Rio de Janeiro alo ng the So utheast Brazilian Continental Margi n. It comprises an approx ima te area of 100,00 km 2 up to 3,400 m Isob ath .Th e Lagoa Feia Form at ion comprises mainly the rift phase sediments of the basin. Intense tecto nic activi ty generated normal faulting with a preferential nor theastern direction and great vert ical displacement. Large basalt flo ws. with ages var ying between 120 Ma and 130 Ma, represent the onset of the rift system forming the basement upon which Lagoa Feia form ation sedime nts were depos ited. The lack of marine fossils indicates non-marin e deposition al environments for this formatio n. The forma tion can be subdivided into four deposi tio n seq uences: Basal Clastic Seq uence. Talc-Srevensltic Sequence. Coquinas Seq uence. and Clastic-Evaporitic Seq uence. Sed iments of the three basa l sequences are indicative of typical lacustrine envi ronments. T he prese nce of talc and stevensite clay-minerals. and the diagenetic assemblage of the Coquinas Sequence sugges t that this lake had alkaline brackis h to saline waters. Alluvial fans and their associated facies deve loped o n the weste rn border and adjace nt to o ther highs o f the basin. Sand flat and mud flat facies compose the marginal portions of the lake. while in deepe r waters hydrocarbon generating shales were deposited. T he Coquinas Sequence rep resents an expressive amount o f pelecipo d calcirudi tes, and calcarenites deposits. which no w are important hydrocar bon reservo irs. An impo rtant and regionally widespread ero sional unconformity separates the Coq uinas Sequence of the overlyin g Clastic-Evaporitic Sequence, which is characteri zed by shallo w water sedimentation defined throu gh stro matolitic and nodu lar limestones associated with extensive deposition of alluvial fans. Th e top o f the Lagoa Feia Formation is marked by a thick evapo ritic layer deposited under hot ar id to sem i-a rid cli mate and relative ly stable tectoni c conditions. con nected with the ocea n at the south. RESUM O ANA LISE SE DIMENTOLOO ICA E EST RAT IGRAF ICA DA FORMA<;AO LAGOA FEIA ESTAGtO Ri FfE DA BACIA DE CAMPOS LlTORAL DO BRAS IL. A Bacia de Cam pos esta situada ao longo do lite ral do Es tado do Rio de Janeiro, Brasil. ocupando urna area de ap roximadamente 100.000 km 2 ate a cola batimetrica de 3.400 m. A Formacao Lagoa Feia engloba os sedimentos depositados dura nte 0 estdglo rift e .A intensa atividadc tcctdni ca desta fase provocou falha mentos de direc;ao preferencial NE e de grandes rejeitos verticals. Bxpre ssivos derrames de roc has basdlticas, com idades entre 120 e 130 Ma , marcam os estag los iniciais da fase rlfte, formand o 0 substrato sobre 0 qual se depositaram os sedimentos da Formacao Lag oa Feia. A ausencia de f6ssei s rnarinhos indica urn ambien te de deposicao nao-marinh o para a forma cao. Esta formacao foi subdivid ida em quatro seq u!nc ias deposiclon ais: Seq uencia Clastics Basal. Seq uencia Ta lco-Es tevensltica, Sequencia d...
In the beginning of exploration of the Brazilian Continental Shelf, Petrobras focused its exploratory efforts on deltaic sequences and a discovery was done in the offshore extension of the Sergipe-Alagoas Basin. The important discoveries in turbidites in Campos Basin in the middle 1970's, pointed out these siliciclastic reservoirs as the main exploratory targets in the Brazilian continental margin. Applying well defined geological models, along with true seismic amplitude and in-house wavelet processing, Petrobras advanced into Campos Basin deep waters in the middle 1980's. Production in such scenery of deep waters and heavy oil was the great challenge to overcome at that time. In the 1990's, the deep water petroleum province in Campos Basin consolidated the Petrobras expertise in Exploration and Production in turbidite reservoirs in the deep and ultra-deep realms. The development of technologies integrating oil and reservoir characterization, drilling systems, artificial lifting and flow technologies were carried out to overcome the challenge of producing from turbidites in deep waters. New geodynamic and geotectonic concepts of rifting have defined new strategies for deep and ultra-deep water areas in Brazilian offshore basins. In Santos basin, these concepts together with seven years of work where the exploratory process was followed according to innovative procedures and adjusted to the geological challenges of the area, Petrobras obtained a tremendous exploratory success and a world-class petroleum province was found. This province is located in the central portion of Santos basin, in ultra deepwater, ranging from 2,000 to less than 3,000 meters water depth and situated about 200 km from the Brazilian coast line. It represents a prominent regional feature covered by a continuous evaporitic sequence, thicker than 2,000 meters. The pre-salt targets comprise a thick carbonate section in depths ranging from 5,000 to 6,500 meters. With the results a paradigm was broken, pointing for the great potential of carbonate rocks in the deep/ultra-deep waters in the Brazilian Continental Margin. New exploratory models and production technologies will be necessary to overcome the challenges that Petrobras will face in near future. Introduction Brazilian petroleum exploration commenced onshore in the Reconcavo Basin in 1948. By the mid 1950s, several small fields had been discovered in the Neocomian/Barremian rift section and by the beginning of the 1960s, exploration of the same rift section led to the discovery of the first onshore Brazilian giant oil field, in the Sergipe Basin. By the mid 1970s, several medium-size fields were found on the continental shelf area of this basin. As an outcome of first oil crisis the exploration of the Brazilian continental margin basins accelerated and by the end of the 1970s, several offshore fields were discovered in the continental shelf of Campos Basin. Intense exploration had then started in Brazil. Petrobras, a government controlled company, rapidly gained experience and developed sedimentological and stratigraphic models for the Brazilian passive continental margin, and its exploration activities moved toward deep water regions. The 1980s were punctuated by the discovery of giant deep water fields in the continental slope region of the Campos Basin (e.g., the Marlim, Albacora, and Caratinga Fields). Very innovative technology was developed to produce from marine siliciclastic reservoirs in this region. The oil-bearing reservoirs are turbidite systems of hyperpicnal origin, deposited in prodelta and deep marine settings. Production from these fields, together with the other Brazilian continental margin fields placed Petrobras as the 9th largest energy company in the world.
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