A methodological evaluation for the efficient investigation of laminated core material collected from the South Pacific islands is presented that is expected to be of broad interest to the core scanning community. Efficient identification of laminae, their number, chemistry and mineralogy provide crucial information in inferring sediment accumulation rates and environmental and climate change. The material investigated was collected as part of NERC grant NE/N006674/1 - The legacy of cyclone Pam: a unique opportunity to build a long term record of cyclone activity in the western tropical Pacific (PIs David Sear, Pete Langdon and Ian Croudace). The project is part of a multi-party study involving the PIs, 3 PhD students and collaborating sp...
Complete data from piston core CD166/19, which was recovered from the Agadir Basin during the RRS Ch...
Eight overlapping sediment cores, representing an approximately 6.6 m–long composite sequence, were ...
In spring 2018, the sediment core TRI1 (38°33'0.61" N, 21°35'20.76" E) was retrieved from 50m water ...
Within the last ten years, micro-XRF (µXRF) core scanning has become an important addition to the su...
This volume presents papers on the use of micro-XRF core scanners in palaeoenvironmental research. I...
The introduction and application of high resolution XRF core scanners has made an enormous contribut...
A procedure is presented for the high-resolution analysis of lake sediment cores. Sections of a sedi...
Micro x-ray fluorescence (µXRF) core scanning is capable of measuring the elemental composition of l...
Marine sediment cores are the fundamental data source for information on seabed character, depositio...
Sediment sampling and treatment Washington Lake (WL): Three sediment cores from the deepest basin we...
This paper describes a method to digitize high-resolution physical properties of annually laminated ...
Marine sediment cores are the fundamental data source for information on seabed character, depositio...
This item is only available electronically.West Basin Lake, in the Western Victorian Volcanic Region...
Laminated sediment records from the oxygen minimum zone in the Arabian Sea offer unique ultrahigh-re...
High-precision depth control is an absolute necessity for varve studies. The Lake Suigetsu 2006 proj...
Complete data from piston core CD166/19, which was recovered from the Agadir Basin during the RRS Ch...
Eight overlapping sediment cores, representing an approximately 6.6 m–long composite sequence, were ...
In spring 2018, the sediment core TRI1 (38°33'0.61" N, 21°35'20.76" E) was retrieved from 50m water ...
Within the last ten years, micro-XRF (µXRF) core scanning has become an important addition to the su...
This volume presents papers on the use of micro-XRF core scanners in palaeoenvironmental research. I...
The introduction and application of high resolution XRF core scanners has made an enormous contribut...
A procedure is presented for the high-resolution analysis of lake sediment cores. Sections of a sedi...
Micro x-ray fluorescence (µXRF) core scanning is capable of measuring the elemental composition of l...
Marine sediment cores are the fundamental data source for information on seabed character, depositio...
Sediment sampling and treatment Washington Lake (WL): Three sediment cores from the deepest basin we...
This paper describes a method to digitize high-resolution physical properties of annually laminated ...
Marine sediment cores are the fundamental data source for information on seabed character, depositio...
This item is only available electronically.West Basin Lake, in the Western Victorian Volcanic Region...
Laminated sediment records from the oxygen minimum zone in the Arabian Sea offer unique ultrahigh-re...
High-precision depth control is an absolute necessity for varve studies. The Lake Suigetsu 2006 proj...
Complete data from piston core CD166/19, which was recovered from the Agadir Basin during the RRS Ch...
Eight overlapping sediment cores, representing an approximately 6.6 m–long composite sequence, were ...
In spring 2018, the sediment core TRI1 (38°33'0.61" N, 21°35'20.76" E) was retrieved from 50m water ...