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generated bysource petroleum reserves % ofworld’stotal O Also showing: Klemme Ulmishek Modified from Rocks Source ceanic (52080104) Assessment Unit Assessment (52080104) chart fortheBaffinBayBasin Appendix 8.Basinevolution 25.0 29.0 12.5 25.0 29.0 12.5 0.2 1.0 9.0 0.3 8.0 0.4 8.0 1.2 2.6 2.8 0.2 1.0 9.0 0.3 8.0 0.4 8.0 1.2 2.6 2.8 A noxic (1990) and E vents Barrett (2003) et Modified from Temperature Global Average Earth Snowball al. (1992)and 15 o Frakes 20 o C Curve Sea Level (1998). (2002) and Modified from 200 Hardenbol Golonka 100 Earth System andothers and Kiessling, 0m Assessment Unit:BaffinBayBasin(52080104) Province: West Greenland–EastCanada

Proterozoic Eon From Geologic TimeScale Era Gradstein

Ediacaran Period andothers(2004) Llandovery Lower Middle

Wenlock Early Late Early Middle Late Ludlow Early Middle Late Middle Early Middle Late Upper Lower Pridoli

Early Middle Late Early Middle Late Moscovian Barremian Visean E M Age 580 560 540 520 500 480 460 440 420 400 380 360 340 320 300 280 260 240 220 200 180 160 140 120 100 80 60 40 20 Ma

Passive Margin Tectonic setting

Small Ocean Basin Basin formation or uplift

Subsidence rate - m/m.y.

2 Basin Evolution 252,000 Km2 Basin area - km Geographic Location:BaffinBayBasin 70 70 70 70 68 68 68 68 66 66 Paleolatitude WT WT NP NP NP NP CT CT CT CT Paleoclimate

H H H H Rate of clastic input

45 45 45 45 45 45 45 45 45 45 Heat flow - mW/m2

Sedimentation and erosion

Elevation/depth - m RSL

Sea Floor Folding, faulting Spreading? and igneous activity

Source rock Petroleum System

Reservoir rock Date: 5/9/08 Compiler: Schenk Seals

Traps

Maturation and migration

Petroleum loss