Seismic stratigraphy, sediments, and basin history of Tonga forearc basin, late Eocene to Pleistocene
Conference
·
· Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:7053430
Four seismic reflectors (A, B, C, V) define primarily unconformity-bounded sedimentary sequences. Basement (V) is a block-faulted surface, apparently of Eocene volcanics. Above this, an upper Eocene sequence (CV) mainly buries the fault topography, pinching out locally on fault-block and volcanic highs along the eastern side of the basin. This sequence includes volcaniclastics and, on paleohighs, shallow-water limestones. Overlying this is a widespread upper Oligocene-lower Miocene sequence (BC), which also thins and pinches out locally against the high eastern side of the basin. Volcaniclastics are common, but limestones may occur locally. Seismic interpretations indicate little faulting during deposition of this sequence; prominent lenticular bodies could be either sills or reefs. Sequence AB, of middle and late Miocene to early Pliocene age, is composed of volcanopelagics deposited when the Lau arc was active, adjacent to the Tonga platform. No volcanic centers are seen in this sequence in the forearc, but shallow intrusions are common. Major tensional faulting developed toward the end of this depositional cycle. The uppermost sequence (SBA), of late Pliocene to Pleistocene age, also comprises volcanopelagic sediments. The volcanics are derived from the nearby Tofua arc, which developed with the opening of the Lau back-arc basin. Doming and tensional faulting in the late Pliocene-Pleistocene raised parts of the Tonga forearc basin, allowing wide reef platforms to develop.
- Research Organization:
- New Zealand Geological Survey, Lower Hutt
- OSTI ID:
- 7053430
- Report Number(s):
- CONF-8608105-
- Conference Information:
- Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 70:7
- Country of Publication:
- United States
- Language:
- English
Similar Records
Evolution of the Izu-Bonin forearc basin
Structure, seismic stratigraphy and petroleum potential of the Tongatapu-'Eua area of the Kingdom of Tonga
Evolution of a forearc basin, Luzon central valley, Philippines
Conference
·
Fri Jun 01 00:00:00 EDT 1990
· AAPG Bulletin (American Association of Petroleum Geologists); (USA)
·
OSTI ID:6165048
Structure, seismic stratigraphy and petroleum potential of the Tongatapu-'Eua area of the Kingdom of Tonga
Conference
·
Fri Jun 01 00:00:00 EDT 1990
· AAPG Bulletin (American Association of Petroleum Geologists); (USA)
·
OSTI ID:6305342
Evolution of a forearc basin, Luzon central valley, Philippines
Journal Article
·
Fri Jul 01 00:00:00 EDT 1983
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:7152807
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
AUSTRALASIA
CARBONATE ROCKS
CENOZOIC ERA
GEOLOGIC AGES
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
GEOPHYSICAL SURVEYS
IGNEOUS ROCKS
LIMESTONE
NEW ZEALAND
ROCKS
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
SEISMIC SURVEYS
SURVEYS
TERTIARY PERIOD
VOLCANIC ROCKS
020200* -- Petroleum-- Reserves
Geology
& Exploration
AUSTRALASIA
CARBONATE ROCKS
CENOZOIC ERA
GEOLOGIC AGES
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
GEOPHYSICAL SURVEYS
IGNEOUS ROCKS
LIMESTONE
NEW ZEALAND
ROCKS
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
SEISMIC SURVEYS
SURVEYS
TERTIARY PERIOD
VOLCANIC ROCKS