PGS 不断推出高质量 GeoStreamer 3D 多传感器地震采集非独家计划，包括记录重力和磁力数据，从而满足了人们对将各种已探明的石油系统和相关油气区类型扩展到坎波斯盆地外部的日益增长的兴趣。 。这一多年期计划将有助于行业对新提供的面积进行评估，扩大深水坎波斯盆地的勘探机会。
这里将根据成像结果和即将进行的巴西招标，介绍盐后和多产盐下部分的勘探潜力。
坎波斯盆地勘探的新地震数据
PGS 最近完成了对巴西近海坎波斯盆地外深水部分 15,600 平方公里多传感器 3D 地震数据的采集。使用多方位角处理将新数据与现有 3D 地震数据相结合，以实现最佳成像，尤其是这个多产油气盆地的盐下结构。该计划符合即将到来的许可轮次（第 17 轮特许权轮次和第七轮共享轮次），符合盐下储层优化地震成像的需求，并阐明了底层石油系统。
E&P Plus: Derisking Presalt Prospectivity in the Deepwater Campos Basin
Improved velocity model accuracy affords improved image quality, illumination and depth accuracy of the subsurface structures found within the presalt play.
Hermann Lebit, John Cramer, Jeffrey Tilton, Yermek Balabekov and Joao Victor Lima, PGS
Learn more about Hart Energy Conferences
Get our latest conference schedules, updates and insights straight to your inbox.
Presented by:
Editor's note: This article originally appeared in the May issue of E&P Plus.
Subscribe to the digital newsletter here.
The outer Campos Basin remains an underexplored domain of the prolific Brazilian hydrocarbon provinces exemplified by super-giant discoveries in the adjacent Santos Basin and in the inner segment of the Campos Basin.
The growing interest in extending the various proven petroleum systems and associated play types into the external Campos Basin is consequentially being answered by PGS with an ongoing non-exclusive program of high-quality GeoStreamer 3D multisensor seismic acquisition, including the recording of gravity and magnetic data. This multiyear program will aid industry evaluation of newly offered acreage, extending the exploration opportunities of the deepwater Campos Basin.
Exploration potential of the post-salt and the prolific presalt section will be presented here in light of the imaging results and the forthcoming Brazil bid round.
New seismic data for Campos Basin exploration
PGS recently completed the acquisition of 15 600 sq km of multisensor 3D seismic data over the deepwater section of the outer Campos Basin offshore Brazil. New data are combined with existing 3D seismic data using multi-azimuth processing to enable optimal imaging particularly of the presalt architecture in this prolific hydrocarbon basin. The program is in line with the forthcoming licensing rounds (Concession Round 17 and 7th Sharing Round), aligns with the demand for optimized seismic imaging of the presalt reservoirs and illuminates the underlying petroleum systems.
In addition, it provides the industry with reliable seismic imaging for appropriate exploration risk mitigation and potential drilling hazard assessment in this emerging deepwater basin.
Campos Basin subsurface setting
The survey covers the entire outer passive margin section of the Campos Basin including large parts of the outboard allochthonous salt edge (Figure 1). Based on the character of the salt architecture and associated structural settings, four major domains have been established. Gravity-driven, thin-skinned tectonics along the basin’s subsiding passive margin, caused prolonged salt movements, which contributed to the formation of these salt structural domains (Figure 1).
PGS Campos Basin 3D Seismic Program
FIGURE 1. Relief of top Aptian evaporites in the deepwater Campos Basin illustrate the major salt tectonic domains (outlined by white dashed lines) and their displacement along a regional sinistral strike-slip fault (red dashed line). Cold colors represent deep, partially welded mini basins. The limit of the allochthonous salt canopy is captured in part by the new 3D seismic acquisition program. (Source: PGS)
An inboard area called the Salt Roller domain refers to the updip zone of post-rift extension that affected the Aptian evaporites and overlying Albian carbonates.
Extension is evident by a network of listric normal faults rooting into the regional decollement along the base of the evaporites. The domain name refers to the predominant salt concentration in triangular-shaped bodies at the footwall of the extensional faults.
The most prolific and giant oil and gas fields of the Campos Basin (e.g., Roncador, Marlim, Jubarte, etc.) reside in the Upper Cretaceous clastic sequences above this salt domain, which might be sourced, at least partially, from presalt hydrocarbon kitchens. Amplitude analysis within the program area revealed similar evidence for hydrocarbon reservoir potential within the postsalt sequence. It further includes promising presalt discoveries near the inner high of the rift system. These are characterized by well-imaged, sag-phase, layered, depositional signatures on-lapping onto tilted fault blocks related to the Lower Cretaceous rifting stages of the margin.
The sag-phase basins contain the rich Barremian source rock sequences while the structural highs are critical for the deposition of the prolific presalt reservoirs, comprising high porosity shallow-water carbonate buildups. The latter are predominantly formed of high energy marine to lacustrine Coquina facies limestones, stromatolitic mounds and sometimes travertine. The drilled sag-phase signature extends beyond the inner high and an adjustment regional ramp, which drops the base of the evaporate sequence over a series of rift-related normal faults (Figure 1).
The slightly deeper outer area is the focus of the new 3D GeoStreamer survey, offering several well imaged hydrocarbon exploration targets underneath the Aptian evaporites. The gentle presalt morphology with structural highs next to stratified sag-basin fills, continues underneath the subsequent two outer salt domains and opens additional exploration running room, where the newly acquired 3D seismic dataset will support exploration and drilling risk mitigation.
Presalt objectives under the Albian Folds and Salt Mini Basins
The Albian Folds domain (Figure 1) is characterized by an intense corrugation at the top of the Aptian evaporite sequence and affects the Albian carbonates. The fold structures quickly dampen against intra-formational unconformities within the Albian carbonate sequence and are caused by early shortening instabilities that appear to be linked to extensional fragmentation of the same sequence at the updip salt roller domain. A line of salt walls, which document the prolonged salt inflation (Figure 1), today separates both domains. Salt movement becomes the dominant condition in the adjacent Mini Basin domain where salt walls and reactive diapirs separate an array of deep mini basins filled with post salt sediments (Figure 1). A few salt bodies transition into active diapirs and reach shallow levels below the mud line, while some of the mini basins are grounded with their Albian sequence against the presalt formation.
Underneath the Mini Basin domain, an approximate North-South trending outer structural high reveals a series of potential presalt reservoirs, more than a half dozen locations already identified by the industry as potential drilling targets (Figure 2). A recent presalt test by Petrobras and partner Exxon Mobil on the Urissane prospect is expected to confirm a working petroleum system and the extension of the presalt play concept into the deepwater sector of the Campos Basin. Petrobras filed a hydrocarbon oil show report to the Brazilian regulator ANP in early first-quarter 2021 on this first outer Campos Basin presalt well.
FIGURE 2. A legacy 3D KPSDM seismic profile along the outer presalt high illustrates post-salt, salt and presalt stratigraphy. Higher quality seismic imaging is required for forthcoming drilling campaigns and appropriate characterization of these promising presalt reservoirs. A recent presalt test by Petrobras (Urissane) and several other permitted presalt well locations are indicated on the graphic. (Source: PGS)
The Outer High and the edge of the salt basin salt kinematics
The outer high forms the proximal shoulder of a l basement graben, underneath thick salt accumulations of the Mini Basin domain (Figure 2). The graben’s distal shoulder images a significant, 1,000-m to 2,000-m basement step that is fragmented by NE-SW trending sinistral transfer fault zones. This basement step likely marks the limit of the passive margin rift system and reveals frequent magmatic features such as sill-like intrusions along the salt base. Beyond the outer basement step the evaporites form an allochthonous salt canopy (Figure 1) that gradually climbs over (possible) Upper Cretaceous deep marine sediment sequences. Analog subsalt plays are well described from other salt basins such as the Northern Gulf of Mexico where significant subsalt discoveries are documented. A portion of this area is included in the acreage offering by ANP in the upcoming Brazil 17th Bidding Round and is covered by the new 3D program.
The geophysical data cover the complete salt kinematic system from the proximal, updip extension to distal compression and salt inflation, including salt mobilization into canopies at the outermost section of the passive margin. It also illuminates the interaction with the underlying rift architecture. The resulting salt kinematics have several implications for hydrocarbon exploration including the top seal assessment for underlying hydrocarbon reservoirs, while the salt architecture impacts seismic wave propagation and therefore the fidelity of the presalt imaging of the reservoirs and their associated petroleum systems.
Advanced seismic technology for presalt imaging
The new data offers a step change in image quality of the emerging Campos presalt play.
Full waveform inversion driven depth velocity modeling of the post-salt, layered evaporate (salt) and presalt sections has provided more accurate velocity model updates by leveraging the full seismic wavefield (reflections and refractions) recorded in these long-offset (10 km) multi-azimuth data. Improved velocity model accuracy affords improved image quality, illumination and depth accuracy of the subsurface structures found within the presalt play. The results will support any future exploration drilling and subsequent reservoir characterization.
