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The giant Chicontepec field contains oil from 18 to 45 oAPI in laminated sandstones of 0.1 to 10 mD at a depth of around 2500 meters (8202 ft). Original Oil in Place (OOIP) is estimated to be 140, 900 MMSTB. The complex geology (complicated structural and stratigraphic nature of the reservoirs), lack of reservoir information and lack of technology availability caused a gap between discovery and development. Throughout a period of several decades some exploration wells were drilled based on 2D seismic and log correlations of the reservoirs. The exploitation of the Paleonchannel was postponed because most of the wells showed poor productivity. The reasons for the low recovery (around 3%) have never been thoroughly understood. Various hypotheses have been proposed to explain the deficient performance such as partial closing of the fractures with declining reservoir pressure (bubble-point pressure is near initial pressure), inadequate comprehension of the geological model, deficiency in the fracturing technology, oil-wetted or intermediate-wetted reservoirs, applicability of unconventional wells (horizontal wells, casing drilling technology), etc. Today, the Chicontepec Paleochannel is an intermediate stage. Due to the experience of different fields with similar characteristics, this paper describes an analysis of alternatives that may be considered to resolve the problems of exploitation at the Chicontepec field. Advanced technologies, hydraulic fractures, artificial lift systems, all of them combined with secondary and enhanced oil recovery, may be feasible to sustain or increase production. A number of hurdles will have to be overcome. This field, the second most important oil field in Mexico, should take advantage of the experience learned from these analogous reservoirs. Chicontepec Paleochannel Geographically, it is located in east-central Mexico in parts of the states of Veracruz, Puebla and Hidalgo. Chincontepec system was deposited under complex tectono-stratigraphic conditions. Geologically, it covers an area of 957,534 acres (Figure 1). Aproximately half of Chicontepec consists of shales or silty shales with the rest of the formation made up of multiple thin sandstones beds and zones of sandstones beds. Typically, between 8 and 16 major reservoirs are present. These set of reservoirs is composed of channel complexes that are flanked by, and rest on, lobe sandstones that grade into distal fan and basin floor deposits, resulting in high heterogeneity. Throughout a period of several decades some exploration wells were drilled based on 2D seismic and log correlations of the reservoirs. The 3D seismic allowed the identification of sand bodies with viable pay thickness. Some wells produce small amounts of water, in general, water-oil contacts have not been identified. X-ray diffraction analysis showed that the clay cointains dominantly kaolinite with a content of 1 to 5 %. The sandstones are immature litharenites consisting of quartz grains, abundant carbonate fragments, and granitic fragments. Because of the abundance of carbonate in the system, the sediments are highly cemented by ferroan calcite and ferroan dolomite, in addition to quartz overgrowths. Core analyses show that the reservoirs are characterized by both low porosity and low permeability, Figure 2. All the reservoirs have permeabilities of 0.1 to 10 mD and porosities ranging from 5 to 15 %. The effective permeability, as determined from build up, fall off, drawdown and step rate test or advance decline analysis, varies from 0.01 to 15 mD.
The giant Chicontepec field contains oil from 18 to 45 oAPI in laminated sandstones of 0.1 to 10 mD at a depth of around 2500 meters (8202 ft). Original Oil in Place (OOIP) is estimated to be 140, 900 MMSTB. The complex geology (complicated structural and stratigraphic nature of the reservoirs), lack of reservoir information and lack of technology availability caused a gap between discovery and development. Throughout a period of several decades some exploration wells were drilled based on 2D seismic and log correlations of the reservoirs. The exploitation of the Paleonchannel was postponed because most of the wells showed poor productivity. The reasons for the low recovery (around 3%) have never been thoroughly understood. Various hypotheses have been proposed to explain the deficient performance such as partial closing of the fractures with declining reservoir pressure (bubble-point pressure is near initial pressure), inadequate comprehension of the geological model, deficiency in the fracturing technology, oil-wetted or intermediate-wetted reservoirs, applicability of unconventional wells (horizontal wells, casing drilling technology), etc. Today, the Chicontepec Paleochannel is an intermediate stage. Due to the experience of different fields with similar characteristics, this paper describes an analysis of alternatives that may be considered to resolve the problems of exploitation at the Chicontepec field. Advanced technologies, hydraulic fractures, artificial lift systems, all of them combined with secondary and enhanced oil recovery, may be feasible to sustain or increase production. A number of hurdles will have to be overcome. This field, the second most important oil field in Mexico, should take advantage of the experience learned from these analogous reservoirs. Chicontepec Paleochannel Geographically, it is located in east-central Mexico in parts of the states of Veracruz, Puebla and Hidalgo. Chincontepec system was deposited under complex tectono-stratigraphic conditions. Geologically, it covers an area of 957,534 acres (Figure 1). Aproximately half of Chicontepec consists of shales or silty shales with the rest of the formation made up of multiple thin sandstones beds and zones of sandstones beds. Typically, between 8 and 16 major reservoirs are present. These set of reservoirs is composed of channel complexes that are flanked by, and rest on, lobe sandstones that grade into distal fan and basin floor deposits, resulting in high heterogeneity. Throughout a period of several decades some exploration wells were drilled based on 2D seismic and log correlations of the reservoirs. The 3D seismic allowed the identification of sand bodies with viable pay thickness. Some wells produce small amounts of water, in general, water-oil contacts have not been identified. X-ray diffraction analysis showed that the clay cointains dominantly kaolinite with a content of 1 to 5 %. The sandstones are immature litharenites consisting of quartz grains, abundant carbonate fragments, and granitic fragments. Because of the abundance of carbonate in the system, the sediments are highly cemented by ferroan calcite and ferroan dolomite, in addition to quartz overgrowths. Core analyses show that the reservoirs are characterized by both low porosity and low permeability, Figure 2. All the reservoirs have permeabilities of 0.1 to 10 mD and porosities ranging from 5 to 15 %. The effective permeability, as determined from build up, fall off, drawdown and step rate test or advance decline analysis, varies from 0.01 to 15 mD.
Chicontepec is associated to a submarine fan system deposited under complex tectono-stratigraphic conditions. Typically, between 8 and 16 major reservoirs are present. These set of reservoirs is composed of channel complexes that are flanked by, and rest on, lobe sandstones that grade into distal fan and basin floor deposits, resulting in high heterogeneity. All the reservoirs have permeabilities of 0.1 to 10 mD and porosities of 5–15 %. Primary recovery by solution gas drive is less than 5 %. The oil density varies from 18 to 45 oAPI depending on his structural position. An aggressive number of well tests were conducted to characterize the fields in Chicontepec. Theses include build up, fall off, drawdown and step rate tests. In recent years, the tests were analyzed to identify well and reservoir factors affecting productivity as well as to determine the effectiveness of well stimulation by fracturing. The typical models used to adjust the information were both vertical fracture and radial homogeneous models. The effective permeability, as determined for these tests and/or advanced decline analysis, ranges from 0.1 to 15 mD. The results seem to indicate that the partial closing of the fractures is caused during the early exploitation. Further analyses suggest that the reservoir rock quality (facies model) along the linear and/or bilinear flow periods having a link with good production rates. This paper presents a relationship found between the effective permeability and the drainage radius. This relationship could be applied to turbidites oil reservoirs with low permeability and low porosity. In order to avoid the interference problems and to optimize new wells, we propose an optimal drainage radius obtained of well test data, pressure-production history and composition fluids. Reservoir Description Geology - Chicontepec Paleochannel, geographically, it is located in east-central Mexico in parts of the states of Veracruz, Puebla and Hidalgo. Chincontepec system was deposited under complex tectono-stratigraphic conditions. Geologically, it is part of the Tampico-Misantla Basin and covers an area of 3875 km2 (Figure 1). Aproximately half of the Chicontepec consists of shales or silty shales with the rest of the formation made up of multiple thin sandstones beds and zones of sandstones beds. Typically, between 8 and 16 major reservoirs are present. These set of reservoirs is composed of channel complexes that are flanked by, and rest on, lobe sandstones that grade into distal fan and basin floor deposits, resulting in high heterogeneity. Facies that are present include channels that can extend from the innerfan to the outer reaches of the fan complex and unconfined fan deposits (lobes) that grade laterally and distally into shelf and basin-floor mudstones, Figure 2. These facies have very distinctive well log shapes (motifs) that allow the identification of environments of deposition of the constructional elements of the fan. Typical facies types are present in fan systems and that have been identified in the Chicontepec are upward coarsening fan deposits, upward fining and blocky channel deposits, interbedded packages and muds of the outer fan that have a serrate gamma ray response, and the muds of the basin floor, Figure 3.
Natural fractures exist in many oil and gas reservoirs. The activation of these fractures can have a significant influence on the initial production and the EUR of the wells. It is therefore very important to know whether they are interconnected and their impact on oil recovery, thus optimizing the development plans of the reservoirs. The giant Chicontepec field, located in central eastern Mexico, with 140 billion barrels of oil in place (OOIP), with laminated turbidite sequences, limited lateral extent, low porosity and permeability, very low current recovery, there are natural fractures or fissures. These natural fractures have been observed in many cores, as well as image logs and outcrops. It is considered that the natural fracture system must be analyzed in Chicontepec in more depth and more importantly, the degree of interconnection may have and its impact on oil recovery because it is estimated that may not be effectively interconnected. Due to the low permeability of the rock, wells are hydraulically fractured. The analysis of the evolution of the pressure at the bottom of the well and or net pressure during a fracturing job is a valuable tool to infer the geometry of the fracture that was generated by the fracturing job. Furthermore, this analysis of the pressure is a powerful tool that can support the identification or existence of interconnected natural fractures and therefore with a certain level of contribution to the producing wells and the recovery of oil from the reservoir. This report presents the application of the analysis of the evolution of the pressure during fracturing jobs in Chicontepec with examples that allow inferring that the natural fractures in Chicontepec are not interconnected or very little.
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