Andaman Islands and Adjoining Offshore: Geology, Tectonics and Palaeoclimate

Inbunden, Engelska, 2020

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This book gathers peer-reviewed research articles on recent advances concerning the geology, geophysics, tectonics, geochronology, sedimentology, igneous petrology, paleo-climate and paleo-oceanography of the Andaman and Nicobar Islands of India and the adjoining ocean basins.

Produktinformation

Utgivningsdatum2020-02-29
Mått155 x 235 x 28 mm
Vikt787 g
FormatInbunden
SpråkEngelska
SerieSociety of Earth Scientists Series
Antal sidor400
Upplaga20001
FörlagSpringer Nature Switzerland AG
ISBN9783030398422

Tillhör följande kategorier

Andaman Ophiolite: An Overview.- Timing of formation and obduction of the Andaman Ophiolite.- Facies stacking of a deep sea depositional lobe: Case study from Paleogene Andaman Flysch, South Andaman Islands, India.- Spatial variation in the composition of Andaman Flysch across the Andaman Islands in relation to source of sediments and tectonics.- Tracing the sources and depositional pathways for the Oligocene sediments in the Andaman Forearc.- Seismicity, lithospheric structure and mantle deformation in the Andaman Nicobar Subduction Zone.- Lithospheric Framework of Sumatra-Andaman Subduction Zone - A Review.- Crustal model for the Andaman Outer Arc: Constraints from Earthquake, Gravity and Receiver Function Data.- Geomagnetic Deep Sounding in Andaman Islands.- On the Trail of the Great 2004 Andaman-Sumatra Earthquake: Seismotectonics and Regional Tsunami History from the Andaman-Nicobar Segment.- A glimpse of crustal deformation through earthquake supercycle in the Andaman region using GPS measurements.- Tectonics of the Andaman Backarc Basin – Present Understanding and Some Outstanding Questions.- Miocene to Pleistocene Palaeoceanography of the Andaman Region: Evolution of the Indian Monsoon on a Warmer-Than-Present Earth.- Late Quaternary Chronostratigraphy, Carbonate Mass Accumulation Rates and Paleoceanography of the Andaman Sea.- Mid to Late Holocene reconstruction of the southwest monsoonal shifts based on a marine sediment core off the Landfall Island, Bay of Bengal.