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Active faults and related Late Quaternary deformation along the Northwestern Himalayan Frontal Zone,India
active faults Northwestern Himalayan Front paleoearthquake thrust and right lateralstrike-slip faults slip-partitioning
2015/9/16
Numerous newly-identified traces of active faults in the Himalayan foothill zone along the HFF around Chandigarh, in Pinjore Dun, along the piedmont zone of the Lower Siwalik hill front and within the...
Late Quaternary history of paleoseismic activity along the Hohhot Segmentof the Daqingshan piedmont faultin Hetao depression zone,North China
Daqingshan piedmont fault (China) Hohhot Segment paleoearthquakes seismichistory completeness of paleoseismic record
2015/9/16
The Daqingshan Piedmont Fault (DPF) is one of the major active normal faults in the Hetao depression zone in the northern part of Ordos Block, North China. It extends in NEE direction along the Daqing...
Late Quaternary activity along the Scorciabuoi Fault (Southern Italy) as inferred from electrical resistivity tomographies
active tectonics Apennines geoelectrical survey Holocene Val d’ Agri
2015/9/2
The Scorciabuoi Fault is one of the major tectonic structures affecting the Southern Apennines, Italy. Across its central sector, we performed several electrical resistivity tomographies with differen...
Damming of River Indus during Late Quaternary in Ladakh Region of Trans-Himalaya, NW India：Implications to Lake formation-climate and tectonics
Late Quaternary Holocene Trans Himalaya Indus Palaeolake deposits climate
2014/1/16
Indus river valley basin in Northwest Indian Himalaya is tectonically unstable, exhibiting a complex topography, landscape relief and varied Quaternary sedimentation. A 422 km transact along the Indus...
Late Quaternary,cryoplanation of rock surfaces in lacustrine environments in the Bergen area,Norway
Late Quaternary cryoplanation rock surfaces lacustrine environments
2009/12/3
Relatively horizontal and smooth rock surfaces bordering lakes 65-150 m a.s.l. in the relatively mountainous Bergen area are described. The surfaces,1- 4 km2 in size and up to 1.5 km wide are develope...
Temporal and spatial variations in Late Quaternary slope sedimentation along the undersupplied margins of the Rockall Trough,offshore west Ireland
Temporal and spatial variations Late Quaternary slope sedimentation undersupplied margins
2009/12/3
A total of 63 gravity cores, together with high-resolution bathymetry data and sidescan sonar imagery, were studied along both eastern and western margins of the Rockall Trough, offshore west Ireland....
Late Quaternary vegetation-climate feedbacks
vegetation-climate feedbacks climate dynamics climate system
2009/12/3
Feedbacks between vegetation and other components of the climate system are discussed with respect to their influence on climate dynamics during the late Quaternary, i.e., the last glacial-interglacia...
A calibrated radiocarbon database of late Quaternary volcanic eruptions
calibrated radiocarbon database late Quaternary volcanic eruptions
2009/10/22
Researchers at the Center for Climatic Research (CCR) at the University of Wisconsin-Madison have revised and calibrated a global volcanic database compiled from more than 2000 radiocarbon-dated erupt...
Synoptic climate change as a driver of late Quaternary glaciations in the mid-latitudes of the Southern Hemisphere
synoptic climate change Quaternary glaciations mid-latitudes Southern Hemisphere
2008/11/10
The relative timing of late Quaternary glacial advances in mid-latitude (40-55° S) mountain belts of the Southern Hemisphere (SH) has become a critical focus in the debate on global climate teleconnec...