Search Results - The Last Tycoon~
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The sedimentary succession of the last ~ 3.50 Myr in the western South Yellow Sea: Paleoenvironmental and tectonic implications
Published 2018“…The depositional succession during the last ~ 3.50 Myr was dominantly controlled by tectonism and glacio-eustatic sea-level cycles. …”
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Ice sheet collapse following a prolonged period of stable sea level during the last interglacial
Published 2013“…Accounting for glacial isostatic adjustment and localized tectonics, we conclude that eustatic sea level rose to about 9 m above present at the end of the last interglacial. …”
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Sedimentary evolution during the last ~1.9 Ma near the western margin of the modern Bohai Sea
Published 2016“…Borehole core YRD-1101 (200.30 m long), drilled in 2011 on the northern coast of the modern Yellow River delta, covers the last ~1.90 Ma, as indicated by paleomagnetic measurements. …”
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SE Asian carbonates: tools for evaluating environmental and climatic change in equatorial tropics over the last 50 million years
Published 2011“…Terrestrial runoff, nutrient upwelling, tectonics, volcanism and recent human activities are major influences on the modern development of carbonate systems. …”
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Structural geology and tectonic history of the Taku Schist and surrounding units, NE Peninsular Malaysia / Muhammad Afiq Md Ali
Published 2018“…In this context, the study demonstrates the structural evolution of the Taku Schist with emphasis on kinematics of shear deformation by way of field and microstructural observations to explain the regional tectonic evolution of NE Peninsular Malaysia. The Taku schist represents an original Paleozoic sedimentary succession metamorphosed to amphibolite facies during Indosinian Orogeny. …”
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Tectonic control on the late stage exhumation of the Aar Massif (Switzerland): Constraints from apatite fission track and (U-Th)/He data
Published 2008“…We explain this accelerated exhumation in the south after ∼3.5 Ma mainly by tectonic denudation in the footwall of the Rhône-Simplon fault and discuss changes in deep crustal configuration, which may have triggered south directed normal faulting. …”
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Constraining mountain front tectonic activity in extensional setting from geomorphology and Quaternary stratigraphy: A case study from the Matese ridge, southern Apennines
Published 2019“…Our study highlights that in the last ∼600 ka, activity along E-W trending normal faults has identified a locus of higher slip rate tectonic activity in the central part of the analysed mountain front. …”
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The geometry and timing of orogenic extension: An example from the western Italian Alps
Published 1999“…The discrete contact zone between eclogite and greenschist facies rocks is the last active part of the GSZ and truncates greenschist facies folds in the footwall. …”
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Is the rate of supercontinent assembly changing with time?
Published 2014“…To address the question of secular changes in the speed of the supercontinent cycle, we use two major databases for the last 2.5 Gyr: the timing and locations of collisional and accretionary orogens, and average plate velocities as deduced from paleomagnetic and paleogeographic data. …”
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Late Quaternary structure and development of the northern Ningaloo Reef, Australia
Published 2003“…Its narrow lagoon is backed by a coastal plain, which is largely composed of an emergent Last Interglacial reef on the flank of folded Tertiary limestones. …”
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Has the impact flux of small and large asteroids varied through time on Mars, the Earth and the Moon?
Published 2022“…The impact flux over the last 3 Ga in the inner Solar System is commonly assumed to be constant through time due to insufficient data to warrant a different choice for this range of time. …”
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Late Tertiary-Quaternary Geological Evolution of the Houtman Abrolhos Carbonate Platforms, Northern Perth Basin
Published 1998“…Coral framestone facies of the Last Interglacial consist mainly of branching coral or head coral, with minor encrusting coralline algae and white lime mud. …”
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Heat fluxes at the Earth's surface and core-mantle boundary since Pangea formation and their implications for the geomagnetic superchrons
Published 2011“…However, the long-term variations of the surface and CMB heat fluxes remain poorly understood, particularly in response to the supercontinent Pangea - likely the most significant global tectonic event in the last 500. Ma. In this study, we reconstruct temporal evolution of the surface and CMB heat fluxes since the Paleozoic by formulating three-dimensional spherical models of mantle convection with plate motion history for the last 450. …”
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