The complex rifting and subsidence history stated earlier has generated a mix of stratigraphy,

Timing and structure conducive to hydrocarbon generation and entrapment (Bell and Campbell, 1990). Up to now, but, significant discoveries only have been situated within a few industries ( ag e.g. Hibernia, Terra Nova, Whiterose) for the northern Jeanne d’Arc basin. Main reservoirs are found in belated Jurassic and Early Cretaceous marine that is shallow fluvial sandstones deposited through the 2nd rift and postrift stages. Later Jurassic shales regarding the Egret member have a source that is marine-rich matured during subsequent burial in the Belated Cretaceous and Tertiary. Traps had been created by the mid- Cretaceous from rollover anticlines ( ag e.g. Hibernia framework) and rotated fault obstructs, and so they had been mostly preserved through the subsequent Avalon uplift and erosion.

Figure 6. Seismic reflection profile 85-4 that is LEKeen and de Voogd, 1988), remigrated and coherency filtered by J. Hall and S. Deemer (individual interaction, 2001). Seismic perspectives identified are Au/A* (Oligocene and Top Cretaceous) and U (Tucholke et al., 1989). Basement crustal kinds are defined by characteristic alterations in expression pattern.

Many exploration has focused from the Jeanne d’Arc basin along with other superficial water basins from the Banking institutions. Just a wells that are few been drilled in much deeper water. Nevertheless, the sediment distribution map (Figure 5a) suggests that significant thicknesses occur beneath many aspects of the increase and slope bordering the Banking institutions ( ag e.g. Southern Whale, Salar, Carson-Bonnition, Flemish Pass and Orphan basins). Recently, extra exploration that is seismic been undertaken during these much much deeper water basins to advance assess its financial potential. Past analysis associated with the much much much deeper regions that are offshore made utilizing several local seismic pages gathered in the mid- 1980’s ( ag e.g. Keen and de Voogd, 1988; Tucholke et al., 1989). A far more current group of local pages (Figure 5) now expands this protection throughout the Newfoundland that is northern basin. The much much deeper water an element of the LE85-4 profile is shown in Figure 6 (J. Hall and S. Deemer, individual interaction, 2001) and a quick section of the current Ewing2000-3 profile (Louden and Lau, 2002) throughout the Carson basin in Figure 7. A few tilted basement fault obstructs is seen as much as 100 kilometer seaward through the rack break. The foremost is a block that is large with a few sodium address that divides the overseas region of the Carson-Bonnition basin into shallower and much much deeper water parts. The deep-water area of thicker sediment and complex cellar framework may keep the potential that is best for hydrocarbons (Enachescu, 1992).

Figure 7. Reflection that is seismic Ewing 2000-3 over the exterior Carson-Bonnition basin showing cellar ridge with possible sodium that separates basin into inner (shallow) from outer (deep water) components.

Seismic perspectives identified are Au/A* and U, after Tucholke et al. (1989). Observe that these horizons pinch out and end against basement and should not be traced into shallower water.

Further seaward for the faulted cellar, a 100-km wide area exists in which a prominent reflector (U) masks the underlying cellar. This reflector seems to end against a number of elevated basement highs. Over the U-reflector, the The u _ A * reflector defines the Tertiary change between flat-lying and bottom present dominated depositional sequences. It isn’t particular in the event that U-reflector is related to your Avalon unconformity regarding the southern Banks and/or the Early Cretaceous ?-reflector observed from the margin that is scotianFigure 4). The type associated with the fairly flat-lying cellar within this transitional area can also be uncertain. Present drilling and seismic outcomes suggest the current presence of a broad area of serpentinized basement that is peridotite a conjugate establishing beneath the Iberia margin (Louden and Lau, 2002). A model that is similar formerly proposed by Enachescu (1992) when it comes to Newfoundland Lesbian dating sites basin. Feasible drilling objectives to resolve these problems have now been selected along profile Ewing 2000-2 in the north area of the basin (Figure 8). A drilling leg of this Ocean Drilling Program is planned because of this work with July-Sept 2003.

Figure 8. Seismic expression profile and location of proposed Ocean Drilling Program drilling web web web sites into the Newfoundland basin (Tucholke et al., 2002). Seismic perspectives Au and U are defined as per Figure 7. For basic location map start to see the Ocean Drilling Program internet site (http: //www-odp. Tamu.edu/publications/tnotes/fy03/210ab. Html)

Into the northwest of Flemish Cap, a rather wide area of dense sediment exists within Orphan basin.

This region experienced rifting episodes that could have extended to the belated Cretaceous. All the basin is underlain by highly thinned continental crust but its deep water has precluded much drilling activity. The gravity highs linked to the rack side (Figure 5b) shows a difference that is significant gravity lows connected with all of the other basins. It has been modeled by changing the reduced crust with mantle, suggesting the existence of a rift that is failed ended up being abandoned whenever continental breakup shifted further into the northeast (Chian et al., 2001). A tremendously sequence that is thick of sediment within the deeper water elements of Orphan basin shows a predominance of post-rift in the place of syn-rift subsidence (Keen and Dehler, 1993).

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