Changes

  | isbn    = 0-89181-602-X

  | isbn    = 0-89181-602-X

}}

}}

Basin paleogeography is defined by picking an isochronous surface or coeval interval and mapping the associated seismic facies and lithofacies. For example, the location of sandy lithofacies vs. clayey lithofacies or mounded vs. tabular seismic reflection configurations may delineate the position of shorelines or reefs. Mapping thickness of reservoir-quality rocks is also useful for establishing paleogeography; thick, linear, dip-oriented trends of sandstone may indicate paleochannel complexes.

Basin paleogeography is defined by picking an isochronous or coeval surface or interval and mapping the associated [[Seismic facies mapping|seismic facies]] and [[lithofacies]]. For example, the location of sandy lithofacies vs. clayey lithofacies or mounded vs. tabular seismic reflection configurations may delineate the position of [[Lithofacies and environmental analysis of clastic depositional systems#Shoreline deposits|shorelines]] or [[reef]]s. Mapping thickness of reservoir-quality rocks is also useful for establishing paleogeography; thick, linear, [[dip]]-oriented trends of sandstone may indicate paleochannel complexes.

==Procedure==

==Procedure==

|-

|-

| 1

| 1

| Identify the stratigraphic interval of a single depositional phase that has potential for containing reservoir rocks, i.e., lowstand or highstand, using biostratigraphic markers and regional correlation surfaces.

| Identify the stratigraphic interval of a single depositional phase that has potential for containing reservoir rocks, i.e., [[Third-order sequences|lowstand or highstand]], using biostratigraphic markers and regional correlation surfaces.

|-

|-

| 2

| 2

| Map depositional facies such as [[Fossil assemblage|biofacies]], net reservoir thickness (lithology or [[porosity]]), and seismic facies (i.e., [[clinoforms]], parallel reflections, chaotic reflections within a single depositional phase).

| Map depositional facies such as [[Fossil assemblage|biofacies]], net reservoir thickness (lithology or [[porosity]]), and [[Seismic facies mapping|seismic facies]] (i.e., [[clinoforms]], parallel reflections, chaotic reflections within a single depositional phase).

|-

|-

| 3

| 3

| Integrate the interpreted seismic facies and biostratigraphic data into a grid of stratigraphic well-log [[cross section]]s if wells are available.

| Integrate the [[Basics of seismic facies analysis|interpreted seismic facies]] and biostratigraphic data into a grid of stratigraphic well-log [[cross section]]s if wells are available.

|-

|-

| 4

| 4

| Map the location of fields producing from reservoirs in the interval of interest with respect to net reservoir thickness; define the type of trap(s) each field contains.

| Map the location of fields producing from reservoirs in the interval of interest with respect to net reservoir thickness; define the type of [[trap]](s) each field contains.

|-

|-

| 5

| 5

| Using the [[seismic interpretation]]s and the geology of the fields mapped in step 4, interpret the deposition of reservoir, seal, and source facies and the formation of stratigraphic or combination traps with respect to sea level cycle phase. Was the reservoir deposited during lowstand, rising, or highstand phases of sea level cycles? What about the seal facies? Is the trap the result of facies relationships that formed during a particular sea level phase or postdepositional [[deformation]]?

| Using the [[seismic interpretation]]s and the geology of the fields mapped in step 4, interpret the deposition of reservoir, seal, and source facies and the formation of stratigraphic or combination traps with respect to [[sea level cycle phase]]. Was the reservoir deposited during lowstand, rising, or highstand phases of sea level cycles? What about the seal facies? Is the trap the result of facies relationships that formed during a particular sea level phase or postdepositional [[deformation]]?

|-

|-

| 6

| 6