generated bysource petroleum reserves % ofworldístotal O Also showing: Klemme Ulmishek Modified from Rocks Source ceanic Assessment Unit: 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 Anoxic (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
Proterozoic Phanerozoic Eon From TimeGeologic Scale Neoproterozoic Paleozoic Mesozoic Cenozoic Era Gradstein
Ediacaran Cambrian Ordovician Silurian Devonian Carboniferous Permian Triassic Jurassic Cretaceous Paleogene Neogene Period andothers(2004) Guadalupian Llandovery Pleistocene Lower Middle Furongian Cisuralian Paleocene Oligocene Pliocene Lopingian Miocene
Wenlock Mississippian Pennsylvanian Early Late Eocene Early Middle Late Working Hypothesis: Ludlow Early Middle Late Middle Early Middle Late Upper Lower Pridoli
Early Middle Late Early Middle Late Epoch Changhsingian Wuchiapingian Pliensbachian Serpukhovian Kimmeridgian Maastrichtian Tremadocian Cenomanian Rhuddanian Serravallian Kasimovian Tournaisian Valanginian Campanian Sinemurian Hauterivian Lochkovian Burdigalian Famennian Sheinwoodian Sakmarian Capitanian Moscovian Hettangian Priabonian Bashkirian Aquitanian Ludfordian Kungurian Barremian Darriwilian Santonian Bathonian Olenekian Berriasian Thanetian Selandian Artinskian Coniacian Oxfordian Bartonian Homerian Tortonian Langhian Callovian Tithonian Telychian Gzhelian Rhaetian Rupelian Turonian Aeronian Aalenian Ypresian Frasnian Asselian Bajocian Wordian Roadian Toarcian Ladinian Chattian Hirnantian Givetian Lutetian Carnian Pragian Paibian Emsian Anisian Eifelian Danian Visean Norian Aptian Albian Messinian Zanclean Gorstian Piacenzian Induan Gelasian 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
Tectonic setting
Basin formation or uplift
Subsidence rate - m/m.y.
Basin area - km2 Basin Evolution
Paleolatitude
Paleoclimate
Rate of clastic input Date:
Heat flow - mW/m2
Sedimentation and erosion
Elevation/depth - m RSL Folding, faulting and igneous activity
Source rock Petroleum System
Reservoir rock
Seals
Traps
Maturation and migration
Petroleum loss Province: Geographic Location: Compiler: Assessment Unit: Working Hypothesis: Date: