Parasequences: Allostratigraphic misfits in sequence stratigraphy
O Catuneanu, M Zecchin - Earth-Science Reviews, 2020 - Elsevier
Parasequences were introduced as the building blocks of seismic-scale systems tracts in the
context of low-resolution seismic stratigraphy. Pitfalls of this concept relate to the definition of …
context of low-resolution seismic stratigraphy. Pitfalls of this concept relate to the definition of …
Accommodation and sediment‐supply controls on clastic parasequences: A meta‐analysis
L Colombera, NP Mountney - Sedimentology, 2020 - Wiley Online Library
This study combines data from many published case studies to undertake a quantitative
characterization of clastic parasequences, with the aim to determine how accommodation …
characterization of clastic parasequences, with the aim to determine how accommodation …
The Quaternary stratigraphic architecture of a low-accommodation, passive-margin continental shelf (Santee Delta region, South Carolina, USA)
JH Long, TJJ Hanebuth… - Journal of …, 2020 - pubs.geoscienceworld.org
The Quaternary stratigraphy of the continental shelf offshore of South Carolina consists of
stratigraphic units deposited in coastal-plain, shallow marine, and shelfal environments …
stratigraphic units deposited in coastal-plain, shallow marine, and shelfal environments …
Flexural deformation controls on Late Quaternary sediment dispersal in the Garo‐Rajmahal Gap, NW Bengal Basin
Subsurface deformation is a driver for river path selection when deformation rates become
comparable to the autogenic mobility rate of rivers. Here we combine geomorphology, soil …
comparable to the autogenic mobility rate of rivers. Here we combine geomorphology, soil …
Cyclic sedimentation in the barakar formation of the Karanpura Field, marginal Gondwana Basin, India
Sequence of strata with consistent and monotonous repetition of two or more kind
alternating lithologies are quite common in geological record through the ages and are …
alternating lithologies are quite common in geological record through the ages and are …
Synchrony evolution of two contradictory prograding Gilbert-type deltas at the margins of the foreland basin (case study from the Neogene Western Carpathian …
D Blaško, S Nehyba - Marine and Petroleum Geology, 2020 - Elsevier
The study concerns about two Miocene deltas located along the opposite margins of the
Western Carpathian Foredeep (peripheral foreland basin), their architecture and evolution …
Western Carpathian Foredeep (peripheral foreland basin), their architecture and evolution …
Sedimentary environment and depositional sequences of the Oligocene Qom Formation in Central Iran based on micro-facies and microtaphofacies analysis
A Safari, H Ghanbarloo, A Kasiri… - Carbonates and …, 2020 - Springer
Oligocene deposits of the Qom Formation in central Iran were studied to reconstruct the
sedimentary environment and depositional sequences based on microfacies (MF) and micro …
sedimentary environment and depositional sequences based on microfacies (MF) and micro …
Analysis of the cyclic character of siliciclastic sediments at the New Jersey continental shelf using ultra-high resolution 3D seismic and well data
M Aali - 2020 - dalspace.library.dal.ca
This dissertation describes the development and application of geophysical techniques to
understand the impact of eustasy on the deposition of shallow-marine stratigraphic …
understand the impact of eustasy on the deposition of shallow-marine stratigraphic …
Dual‐system tract pattern: Significance for foreland basin reservoir prediction (Jurassic, Central Junggar Basin, West China)
XB Du, P Chen, Y Lu, X Song - Geological Journal, 2020 - Wiley Online Library
The Junggar Basin is a typical superimposed system characterized by multilateral steep
thrusts and extrusions and one of the primary petroliferous basins in Western China. To …
thrusts and extrusions and one of the primary petroliferous basins in Western China. To …
[PDF][PDF] HNIDON AREA, KYAIKMARAW TOWNSHIP, MON STATE
NM Maung, DW Aung, TT Zaw - maas.edu.mm
The study area is situated in the southeastern part of Kyaikmaraw Township, Mon State. It
lies between latitude 16º 20'30" N to 16º 23'00" N and longitude 97º44'42" E to 97º 47'24" E …
lies between latitude 16º 20'30" N to 16º 23'00" N and longitude 97º44'42" E to 97º 47'24" E …