114 research outputs found
Current thoughts on the beginnings of food-production in southwestern Asia
No full textBraidwood Linda S., Braidwood Robert J. Current thoughts on the beginnings of food-production in southwestern Asia. In: Mélanges de l'Université Saint-Joseph, tome 45, 1969. Mélanges offerts à M. Maurice Dunand. Tome I. pp. 147-155
The University of Chicago Oriental Institute Publications, Volume LXI, Excavations in the plain of Antioch. I, The earlier assemblage. Phases A-J. by Robert J. Braidwood a. Linda S. Braidwood. The University of Chicago Press, Chicago, Illinois, 1960
No full textTallon M. The University of Chicago Oriental Institute Publications, Volume LXI, Excavations in the plain of Antioch. I, The earlier assemblage. Phases A-J. by Robert J. Braidwood a. Linda S. Braidwood. The University of Chicago Press, Chicago, Illinois, 1960. In: Mélanges de l'Université Saint-Joseph, tome 36, 1959. pp. 199-201
GSNSW Exploration NSW Area S Braidwood uranium grid geodetic
No full textMaintenance and Update Frequency: notPlannedStatement: This GSNSW Exploration NSW Area S Braidwood uranium grid geodetic is an airborne-derived radiometric uranium grid for the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001. The survey was acquired under the project No. 756 for the geological survey of NSW. The grid has a cell size of 0.00049 degrees (approximately 50m). A total of 25736 line-kilometres of data at a line spacing of 250m and 60m terrain clearance were acquired to produce this grid. This radiometric uranium grid shows uranium element concentration of the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 in units of parts per million (or ppm). Noise-adjusted singular value decomposition (NASVD) has been applied to the data. NASVD is a spectral component analysis procedure for the removal of noise from gamma-ray spectra. Details of the specifications of individual airborne surveys can be found in the Fourteenth Edition of the Index of Airborne Geophysical Surveys (Percival, 2014). This Index is also available online at http://pid.geoscience.gov.au/dataset/79134.
Reference:
Percival, P.J., 2014. Index of airborne geophysical surveys (Fourteenth Edition).The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive decay of potassium (K), uranium (U) and thorium (Th). The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.<br/>This radiometric uranium grid has a cell size of 0.00049 degrees (approximately 50m) and shows uranium element concentration of the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 in units of parts per million (or ppm). The data used to produce this grid was acquired in 2001 by the NSW Government, and consisted of 25736 line-kilometres of data at 250m line spacing and 60m terrain clearance
GSNSW Exploration NSW Area S Braidwood potassium grid geodetic
No full textMaintenance and Update Frequency: notPlannedStatement: This GSNSW Exploration NSW Area S Braidwood potassium grid geodetic is an airborne-derived radiometric potassium grid for the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001. The survey was acquired under the project No. 756 for the geological survey of NSW. The grid has a cell size of 0.00049 degrees (approximately 50m). A total of 25736 line-kilometres of data at a line spacing of 250m and 60m terrain clearance were acquired to produce this grid. This radiometric potassium grid shows potassium element concentration of the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 in units of percent (or %). Noise-adjusted singular value decomposition (NASVD) has been applied to the data. NASVD is a spectral component analysis procedure for the removal of noise from gamma-ray spectra. Details of the specifications of individual airborne surveys can be found in the Fourteenth Edition of the Index of Airborne Geophysical Surveys (Percival, 2014). This Index is also available online at http://pid.geoscience.gov.au/dataset/79134.
Reference:
Percival, P.J., 2014. Index of airborne geophysical surveys (Fourteenth Edition).The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive decay of potassium (K), uranium (U) and thorium (Th). The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.<br/>This radiometric potassium grid has a cell size of 0.00049 degrees (approximately 50m) and shows potassium element concentration of the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 in units of percent (or %). The data used to produce this grid was acquired in 2001 by the NSW Government, and consisted of 25736 line-kilometres of data at 250m line spacing and 60m terrain clearance
GSNSW Exploration NSW Area S Braidwood thorium grid geodetic
No full textMaintenance and Update Frequency: notPlannedStatement: This GSNSW Exploration NSW Area S Braidwood thorium grid geodetic is an airborne-derived radiometric thorium grid for the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001. The survey was acquired under the project No. 756 for the geological survey of NSW. The grid has a cell size of 0.00049 degrees (approximately 50m). A total of 25736 line-kilometres of data at a line spacing of 250m and 60m terrain clearance were acquired to produce this grid. This radiometric thorium grid shows thorium element concentration of the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 in units of parts per million (or ppm). Noise-adjusted singular value decomposition (NASVD) has been applied to the data. NASVD is a spectral component analysis procedure for the removal of noise from gamma-ray spectra. Details of the specifications of individual airborne surveys can be found in the Fourteenth Edition of the Index of Airborne Geophysical Surveys (Percival, 2014). This Index is also available online at http://pid.geoscience.gov.au/dataset/79134.
Reference:
Percival, P.J., 2014. Index of airborne geophysical surveys (Fourteenth Edition).The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive decay of potassium (K), uranium (U) and thorium (Th). The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.<br/>This radiometric thorium grid has a cell size of 0.00049 degrees (approximately 50m) and shows thorium element concentration of the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 in units of parts per million (or ppm). The data used to produce this grid was acquired in 2001 by the NSW Government, and consisted of 25736 line-kilometres of data at 250m line spacing and 60m terrain clearance
GSNSW Exploration NSW Area S Braidwood magnetic grid geodetic
No full textMaintenance and Update Frequency: notPlannedStatement: This GSNSW Exploration NSW Area S Braidwood magnetic grid geodetic is an airborne-derived Total Magnetic Intensity (TMI) grid for the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 survey. The survey was acquired under the project No. 756 for the geological survey of NSW. The grid has a cell size of 0.00049 degrees (approximately 50m). The units are in nanoTesla (or nT). A total of 25736 line-kilometres of data at a line spacing of 250m and 60m terrain clearance were acquired to produce this grid. Details of the specifications of individual airborne surveys can be found in the Fourteenth Edition of the Index of Airborne Geophysical Surveys (Percival, 2014). This Index is also available online at http://pid.geoscience.gov.au/dataset/79134.
Reference:
Percival, P.J., 2014. Index of airborne geophysical surveys (Fourteenth Edition).Total magnetic intensity (TMI) data measures variations in the intensity of the Earth's magnetic field caused by the contrasting content of rock-forming minerals in the Earth crust. Magnetic anomalies can be either positive (field stronger than normal) or negative (field weaker) depending on the susceptibility of the rock. The data are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.<br/>This GSNSW Exploration NSW Area S Braidwood magnetic grid geodetic has a cell size of 0.00049 degrees (approximately 50m). The units are in nanoTesla (or nT). The data used to produce this grid was acquired in 2001 by the NSW Government, and consisted of 25736 line-kilometres of data at 250m line spacing and 60m terrain clearance
Braidwood Gravity Survey 2006 (P200620), gravity point data
No full textMaintenance and Update Frequency: notPlannedStatement: This Braidwood Gravity Survey 2006 (P200620), gravity point data contains ground gravity point data for the Braidwood Gravity Survey 2006 (P200620) survey acquired for Geological Survey of New South Wales (GSNSW). This dataset contains a total of 917 point data values. The data is located in NSW and were acquired in 2006. The point located data were collected in grid layout at a station spacing between 1000 and 2000 metres.
Terrain corrections were calculated using the INTREPID Geophysics software package. The processed data are checked by GA geophysicists using standard methods for assessing quality to ensure that the final data are fit-for-purpose.
All data are provided in EPSG:4283 coordinates, Australian Height Datum (AHD) and gravity datum of AAGD07. The units are degrees, meters, and micrometres per second squared, respectively.
Reference:
Intrepid Geophysics, http://www.intrepid-geophysics.com.Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.<br/> This Braidwood Gravity Survey 2006 (P200620) contains a total of 917 point data values acquired at a spacing between 1000 and 2000 metres. The data is located in NSW and were acquired in 2006, under project No. 200620 for Geological Survey of New South Wales (GSNSW)
FIGURE 97–111 in Small diatoms (Bacillariophyta) in cultures from the Styx River, New Zealand, including descriptions of three new species
No full textFIGURE 97–111. Navicula veneta, strain LCR-S:2:2:1, CHR618416. Scales: Fig 97, 10 µm; Fig. 98, 5 µm (use for Figs 98–104); Fig. 109, 1 µm (use for Figs 106–109), all others 1 µm. Fig. 97. Live cells viewed by LM, showing paired parietal plastids close against valve margins. Fig. 98–104. Cleaned frustules viewed by LM (girdle view in Fig. 104). Figs 105–111. SEM of cleaned frustules. Fig. 105, whole frustule, showing elongated, longitudinally aligned areolae; Figs 106–109, widened central area of four valves, showing hooked central raphe termini; Figs 110, 111, valve apices showing hooked raphe termini and pattern of areolae.Published as part of Novis, Phil M., Braidwood, Jasmine & Kilroy, Cathy, 2012, Small diatoms (Bacillariophyta) in cultures from the Styx River, New Zealand, including descriptions of three new species, pp. 11-45 in Phytotaxa 64 (1) on page 32, DOI: 10.11646/phytotaxa.64.1.3, http://zenodo.org/record/506200
NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 (P756), magnetic line data, AWAGS levelled
No full textMaintenance and Update Frequency: notPlannedStatement: This NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 (P756), magnetic line data, AWAGS levelled is an airborne-derived magnetic line dataset for the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 survey. The data was acquired under the project No. 756 for the geological survey of NSW. A total of 25736 line-kilometres of data at a line spacing of 250m and 60m terrain clearance were acquired during this survey. To constrain long wavelengths in the data, an independent data set, the Australia-wide Airborne Geophysical Survey (AWAGS) airborne magnetic data, was used to control the base levels of the survey data (Milligan et al., 2009). This survey data is essentially levelled to AWAGS. Details of the specifications of individual airborne surveys can be found in the Fourteenth Edition of the Index of Airborne Geophysical Surveys (Percival, 2014). This Index is also available online at http://pid.geoscience.gov.au/dataset/79134.
References:
Milligan, P.R., Minty, B.R.S., Richardson, M. & Franklin, R., 2009. The Australia-wide Airborne Geophysical Survey accurate continental magnetic coverage. Preview, No. 138, p. 1-128,
Percival, P.J., 2014. Index of airborne geophysical surveys (Fourteenth Edition).Total magnetic intensity (TMI) data measures variations in the intensity of the Earth's magnetic field caused by the contrasting content of rock-forming minerals in the Earth crust. Magnetic anomalies can be either positive (field stronger than normal) or negative (field weaker) depending on the susceptibility of the rock. The data are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.<br/> These line dataset from the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 survey were acquired in 2001 by the NSW Government, and consisted of 25736 line-kilometres of data at 250m line spacing and 60m terrain clearance. To constrain long wavelengths in the data, an independent data set, the Australia-wide Airborne Geophysical Survey (AWAGS) airborne magnetic data, was used to control the base levels of the survey data. This survey data is essentially levelled to AWAGS
NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 (P756), radiometric line data, AWAGS levelled
No full textMaintenance and Update Frequency: notPlannedStatement: This NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 (P756), radiometric line data, AWAGS levelled is an airborne-derived radiometric data for the NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001. The data was acquired under the project No. 756 for the geological survey of NSW. A total of 25736 line-kilometres of data at a line spacing of 250m were acquired during this survey. To constrain long wavelengths in the data, an independent data set, the Australia-wide Airborne Geophysical Survey (AWAGS) airborne magnetic data, was used to control the base levels of the survey data (Milligan et al., 2009). This survey data is essentially levelled to AWAGS. Noise-adjusted singular value decomposition (NASVD) has been applied to the data. NASVD is a spectral component analysis procedure for the removal of noise from gamma-ray spectra. Details of the specifications of individual airborne surveys can be found in the Fourteenth Edition of the Index of Airborne Geophysical Surveys (Percival, 2014). This Index is also available online at http://pid.geoscience.gov.au/dataset/79134.
References:
Milligan, P.R., Minty, B.R.S., Richardson, M. & Franklin, R., 2009. The Australia-wide Airborne Geophysical Survey accurate continental magnetic coverage. Preview, No. 138, p. 1-128,
Percival, P.J., 2014. Index of airborne geophysical surveys (Fourteenth Edition).The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive decay of potassium (K), uranium (U) and thorium (Th). The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.<br/> This NSW DMR, Discovery 2000, Area S, Braidwood, NSW 2001 (P756), radiometric line data, AWAGS levelled were acquired in 2001 by the NSW Government, and consisted of 25736 line-kilometres of data at 250m line spacing and 60m terrain clearance. To constrain long wavelengths in the data, an independent data set, the Australia-wide Airborne Geophysical Survey (AWAGS) airborne magnetic data, was used to control the base levels of the survey data. This survey data is essentially levelled to AWAGS
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