Four-dimensional analog and geometrical modeling of the Hides anticline, Papua New Guinea: Structure of a giant gas field
Abstract
The Hides anticline in the Papua New Guinea fold belt is the core part of the Papua New Guinea liquified natural gas project that commenced production in 2014, yet little is known about its internal structure, particularly at depth. The structure of the upper 3 km (9843 ft) is relatively well constrained from surface data, recent development wells, and poor-quality two-dimensional seismic data, but the deep structure has been obscure. Seismic data and gravity modeling suggest an underlying large normal fault in basement. Forward geometrical modeling using MoveTM and four-dimensional analog sandbox modeling under an x-ray tomography scanner have greatly constrained the structural interpretation. The modeling confirms the presence of the underlying basement normal fault and suggests that it was mildly inverted prior to the onset of pure compression deformation in the sedimentary section. The main detachment level was just above basement approximately 8–10 km (∼5–6 mi) beneath the surface, but this ramped up at the basement fault creating an array of triangle-zone faults through the overlying sedimentary section, building the Hides anticline. The early inversion was instrumental in initiating a back thrust and hinterland-verging tight fold in the Mesozoic section, including the source, reservoir, and seal. Deformation in the thick Miocene carbonates at the surface was detached from that in the underlying reservoir along an Upper Cretaceous mudstone horizon that varies strongly in thickness such that the 2–4-km (6562–13,123-ft)-high Mesozoic structure verges northeast and the overlying Miocene structure verges southwest. Analog modeling shows that a ductile stratigraphy is required with slow strain rates of approximately 1–3 km/m.y. (∼3281–9843 ft/m.y.).
Keywords
Miocene
models
Mesozoic
kinematics
history
giant fields
geophysical surveys
geophysical profiles
rheology
sedimentary rocks
development
depth
compression tectonics
clastic rocks
Cenozoic
carbonate rocks
basement tectonics
Australasia
ductile deformation
faults
errors
deformation
Cretaceous
crustal shortening
seismic methods
seismic profiles
source rocks
surveys
tectonics: Tertiary: thickness
thin-skinned tectonics
three-dimensional models
triangle zones
Upper Cretaceous
velocity
X-ray data
Darai Limestone
Juha Anticline
Hides Field
P'nyang Anticline
Hides Anticline
Tagari Valley
geophysical methods
geometry
four-dimensional models
reservoir rocks
petroleum exploration
petroleum
Papua New Guinea
oil wells
oil and gas fields
Neogene
normal faults
natural gas
mudstone