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High-resolution sequence stratigraphy (HRSS) is a new way for layer correlation.
High-resolution sequence stratigraphic analysis shows to be parasequences the smallest depositional packages (metre-scale cycles) within the platforms.
Such linkage of eustatic, biological and isotopic records to the climatically forced development of an ice sheet can only be contemplated within a framework of high-resolution sequence stratigraphy that integrates allo-, chemor or biostratigraphic markers.
It defines the building blocks of a prograding avulsion sequence from a high-resolution sequence stratigraphy perspective, proposes concepts in non-marine sequence stratigraphy and flood basin evolution, and defines the continental equivalent to a parasequence.
In this context, we present a regional, high-resolution sequence stratigraphic framework for the Brent Group, UK North Sea based on extensive sedimentological re-interpretation of core and wireline-log data, combined with palynostratigraphy and published literature.
Outcrop-based study of high-resolution sequence stratigraphy (intra- and interfacies sedimentologic clues) in Neoproterozoic Lakheri Limestone, Central India, reveals definite signals for relative sea level variations and paleogeographic shifts between shallow beach-shoreface and distal-shelf.
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In this study, we examined the sedimentary response of the Po Plain coastal system to short-term (millennial-scale) relative fluctuations of sea level through high-resolution sequence-stratigraphic analysis of the Holocene succession.
These enable tracking of the maximum flooding surface into its updip (lagoonal/estuarine) counterpart, thus highlighting the role of refined palaeontological criteria as a powerful tool for high-resolution sequence-stratigraphic studies.
The post-PCR technologies that are used to provide information are selected based on the objective of the assay and they range from simple indirect size-based approaches such as gel electrophoresis to high-resolution sequence-based analyses of the entire genome.
This paper demonstrates field relationships between landforms, facies, and high-resolution sequences in avulsion deposits.
In the mid-eastern Yellow Sea, late Pleistocene Holocene glacio-eustatic sea-level fluctuations and a local subsidence regime have formed an aggradational set of high-resolution sequences (sequences I V in descending order).
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