Fault trap regime

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Exploring for Oil and Gas Traps
Series Treatise in Petroleum Geology
Part Traps, trap types, and the petroleum system
Chapter Classification of exploration traps
Author Richard R. Vincelette, Edward A. Beaumont, Norman H. Foster
Link Web page
Store AAPG Store

Classes and definitions

There are four classes in the fault trap regime: normal fault, reverse fault, thrust fault, and wrench fault. The outline below shows definitions and examples for the classes and subclasses of these traps or trapping elements.

Regime: Fault trap
Fault(s) forms part or all of the closure of the trap by sealing the reservoir either laterally and/or from the top (after Biddle and Wielchowsky, 1995).

Class: Normal fault trap
One or more form all or part of lateral closure by sealing the reservoir.
Subclass: Tilted fault block
Block of rock bounded on one or more sides by normal faults. Rotation traps hydrocarbons along edges or in corners.
Subclass: Horst
Block of rock bounded on all sides by normal faults.
Subclass: Listric fault trap
All or part of closure formed by a fault whose plane curves downward and is concave upward.
Class: Reverse fault trap
One or more faults form all or part of the closure by sealing the reservoir.
Class: Thrust fault trap
Forms all or part of the closure by sealing the reservoir either laterally or from the top or bottom.
Subclass: Overthrust
Forms all or part of the closure by sealing the reservoir laterally.
Subclass: Subthrust
Forms all or part of the closure by sealing the reservoir laterally or from the top.
Class: Wrench fault trap
Forms all or part of the closure by sealing the reservoir laterally or from the top.
Subclass: Flower structure
Opposing reverse faults diverge upward, forming a fan or flower cross section pattern. Develop along wrench fault zones.

Families

Based on the genesis of the bounding faults, traps classified as fault traps can be divided into tectonic and nontectonic superfamilies. The outline below presents examples of trap families for several common fault traps. Similar trap families and subfamilies can be defined for most fault traps when the genesis of the trap is understood fully.

Regime: Fault traps

Class: Normal faults
Subclass: Tilted fault block
Superfamily: Tectonic
Normal fault, resulting from deformation by tectonic processes, forms all or part of the closure.
Family: Extensional
Fault, resulting from extensional deformation, forms all or part of the closure.
Subfamily: Rift basin
Subfamily: Basin and range
Subfamily: Growth fault
Class: Reverse faults
Subclass: Thrust faults
Superfamily: Tectonic
Thrust fault, resulting from tectonic deformation by tectonic processes, forms all or part of the closure.
Family: Compressional
Fault, resulting from tectonic compressional deformation, forms all or part of the closure.
Subfamily: Regional thrust belt
Subfamily: Foreland fold fault
Subfamily: Forearc basin
Class: Wrench faults
Subclass: Flower structures
Superfamily: Tectonic
Normal fault, resulting from tectonic deformation by tectonic processes, forms all or part of the closure.
Family: Transpressional
Fault, resulting from tectonic transpressional deformation, forms all or part of the closure.
Subfamily: Regional wrench system
Variety: Inverted
Class: Normal faults
Superfamily: Nontectonic
Result from deformation by nontectonic processes such as uplift by intrusion or diapirism, differential compaction, salt withdrawal, salt solution, or meteoric impact.
Family: Extensional
Fault, resulting from nontectonic extensional deformation, forms all or part of the closure.
Family: Vertical uplift
Family: Vertical subsidence
Subfamily: Salt solution
Subfamily: Salt withdrawal

See also

External links

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Fault trap regime
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