cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.15366992
title: Table 7 C in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 7C. Locality data, analysed rocks, Tumbarumba-Cabramurra basalts.
DR14639Coarse grained olivine-rich alkali basalt flow, Yorker’s Creek, 1120 m R.L., Ravine 1:25 000 Sheet (GR 193 395)DR13822Coarse olivine basalt (micro-dolerite) plug (?), Ruby Creek, 950 m R.L., Tumbarumba 1:25 000 Sheet (GR 075 352)DR13835Basanite flow, Link Road, west of Ravine Junction, 1325 m R.L., Cabramurra 1: 25 000 Sheet (GR 274 287)DR14650Vesicular olivine-pyroxene phyric basanite, Rutherford Ridge, 1275 m R.L., Courabyra 1:25 000 Sheet (GR 060 539)DR13820Vesicular olivine-pyroxene phyric basanite, 0.7 km NE of Courabyra-Adelong road junction, 860 m R.L., Courabyra 1:25 000 Sheet (GR 947 507)DR14662Columnar olivine-pyroxene phyric basanite, lowest flow, Bald Hill, Tooma-Tumbarumba Road, 460 m R.L., Tooma 1:25 000 Sheet (GR 971 202)DR13828Columnar olivine alkali basalt flow, Laurel Hill camp, Adelong Road, 1000 m R.L., Courabyra 1:25 000 Sheet (GR 965 563) *DR14641Flow banded olivine-pyroxene phyric basanite, W side Jimmies Road, near Granite Mountain, 1360 m R.L., Courabyra 1:25 000 Sheet (GR 090 458)IG159Massive olivine basalt flow, near Talbingo, 1030 m R.L., Yarrangobilly 1:25 000 Sheet (GR 139 545)SL61Basanite flow, Ruby Creek, 1060 m R.L., Tumbarumba 1:25 000 Sheet (GR 096 374)SL62Olivine alkali basalt flow, above Ruby Creek, 1010 m R.L. Tumbarumba 1:25 000 Sheet (GR 073 359)
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 231 in Records of the Australian Museum 54 (2) on page 231, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15366991
title: Table 7 C in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 7C. Locality data, analysed rocks, Tumbarumba-Cabramurra basalts.
DR14639Coarse grained olivine-rich alkali basalt flow, Yorker’s Creek, 1120 m R.L., Ravine 1:25 000 Sheet (GR 193 395)DR13822Coarse olivine basalt (micro-dolerite) plug (?), Ruby Creek, 950 m R.L., Tumbarumba 1:25 000 Sheet (GR 075 352)DR13835Basanite flow, Link Road, west of Ravine Junction, 1325 m R.L., Cabramurra 1: 25 000 Sheet (GR 274 287)DR14650Vesicular olivine-pyroxene phyric basanite, Rutherford Ridge, 1275 m R.L., Courabyra 1:25 000 Sheet (GR 060 539)DR13820Vesicular olivine-pyroxene phyric basanite, 0.7 km NE of Courabyra-Adelong road junction, 860 m R.L., Courabyra 1:25 000 Sheet (GR 947 507)DR14662Columnar olivine-pyroxene phyric basanite, lowest flow, Bald Hill, Tooma-Tumbarumba Road, 460 m R.L., Tooma 1:25 000 Sheet (GR 971 202)DR13828Columnar olivine alkali basalt flow, Laurel Hill camp, Adelong Road, 1000 m R.L., Courabyra 1:25 000 Sheet (GR 965 563) *DR14641Flow banded olivine-pyroxene phyric basanite, W side Jimmies Road, near Granite Mountain, 1360 m R.L., Courabyra 1:25 000 Sheet (GR 090 458)IG159Massive olivine basalt flow, near Talbingo, 1030 m R.L., Yarrangobilly 1:25 000 Sheet (GR 139 545)SL61Basanite flow, Ruby Creek, 1060 m R.L., Tumbarumba 1:25 000 Sheet (GR 096 374)SL62Olivine alkali basalt flow, above Ruby Creek, 1010 m R.L. Tumbarumba 1:25 000 Sheet (GR 073 359)
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 231 in Records of the Australian Museum 54 (2) on page 231, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15366993
title: Table 8 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 8. Summary of SHRIMP U-Pb zircon results for Tumbarumba sapphires.
sample no. grain · spot204 Pb/ 206 Pbf 206f 206 %totaltotalradiogenicage (Ma)238 U/ 206 Pb ±207 Pb/ 206 Pb ±206 Pb/ 238 U ±206 Pb/ 238 U ±C461 · 10.0000411.15E-021.1519.960.2400.06190.00070.04950.0006311.63.72 · 10.0000145.03E030.5015.880.1790.05880.00040.06270.0007391.74.33 · 10.0001001.77E-030.1822.160.3280.05350.00050.04510.0007284.04.14 · 10.0000152.61E-030.2623.840.2620.05370.00040.04180.0005264.22.95 · 10.0000100.002160.2223.090.2610.05360.00050.04320.0005272.73.0C631 · 10.0008351.35E-021.35230.102.7470.05720.00110.00430.000127.60.31 · 20.0010571.01E-021.01275.603.9410.05440.00200.00360.000123.10.31 · 30.0000400.005890.597.080.0860.07230.00050.14040.0017846.79.72 · 10.0037390.09238.2387.581.1340.11240.00140.01050.000167.20.92 · 20.0005670.008060.81279.983.6210.05290.00170.00350.000122.80.33 · 10.0018940.015311.53280.334.8870.05860.00380.00350.000122.60.43 · 20.0000111.26E-03<0.016.660.0800.06770.00040.15030.0018902.710.2
Uncertainties given at the one level. f % denotes the percentage of 206 Pb that is common Pb
206 Correction for common Pb made using the measured 238 U/ 206 Pb and 207 Pb ratios following Tera & Wasserburg (1972) as outlined in Compston et al. (1992). U, Th, Pb* contents (ppm) (* = total radiogenic Pb).
C46: 1.1 U 936, Th 428, Th/U 0.48, Pb 34; 2.1 U 1048, Th 193, Th/U 0.18, Pb 49; 3.1 U 1191, Th 353, Th/U 0.30, Pb 40; 4.1 U 1081, Th 320, Th/U 0.30, Pb 33; 5.1 U 1139, Th 409, Th/U 0.36, Pb 37.
C63: 1.1 U 1454, Th 1227, Th/U 0.84, Pb 6; 1.2 U 861, Th 627, Th/U 0.73, Pb 3; 1.3 U 623, Th 212, Th/U 0.34, Pb 71; 2.1 U 867, Th 552, Th/U 0.64, Pb 7; 2.2 U 812, Th 1219, Th/U 1.50, Pb 3; 3.1 U 301, Th 524, Th/U 1.74, Pb 1; 3.2 U 573, Th 230, Th/U 0.40, Pb 72.
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 234 in Records of the Australian Museum 54 (2) on page 234, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15366994
title: Table 8 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 8. Summary of SHRIMP U-Pb zircon results for Tumbarumba sapphires.
sample no. grain · spot204 Pb/ 206 Pbf 206f 206 %totaltotalradiogenicage (Ma)238 U/ 206 Pb ±207 Pb/ 206 Pb ±206 Pb/ 238 U ±206 Pb/ 238 U ±C461 · 10.0000411.15E-021.1519.960.2400.06190.00070.04950.0006311.63.72 · 10.0000145.03E030.5015.880.1790.05880.00040.06270.0007391.74.33 · 10.0001001.77E-030.1822.160.3280.05350.00050.04510.0007284.04.14 · 10.0000152.61E-030.2623.840.2620.05370.00040.04180.0005264.22.95 · 10.0000100.002160.2223.090.2610.05360.00050.04320.0005272.73.0C631 · 10.0008351.35E-021.35230.102.7470.05720.00110.00430.000127.60.31 · 20.0010571.01E-021.01275.603.9410.05440.00200.00360.000123.10.31 · 30.0000400.005890.597.080.0860.07230.00050.14040.0017846.79.72 · 10.0037390.09238.2387.581.1340.11240.00140.01050.000167.20.92 · 20.0005670.008060.81279.983.6210.05290.00170.00350.000122.80.33 · 10.0018940.015311.53280.334.8870.05860.00380.00350.000122.60.43 · 20.0000111.26E-03<0.016.660.0800.06770.00040.15030.0018902.710.2
Uncertainties given at the one level. f % denotes the percentage of 206 Pb that is common Pb
206 Correction for common Pb made using the measured 238 U/ 206 Pb and 207 Pb ratios following Tera & Wasserburg (1972) as outlined in Compston et al. (1992). U, Th, Pb* contents (ppm) (* = total radiogenic Pb).
C46: 1.1 U 936, Th 428, Th/U 0.48, Pb 34; 2.1 U 1048, Th 193, Th/U 0.18, Pb 49; 3.1 U 1191, Th 353, Th/U 0.30, Pb 40; 4.1 U 1081, Th 320, Th/U 0.30, Pb 33; 5.1 U 1139, Th 409, Th/U 0.36, Pb 37.
C63: 1.1 U 1454, Th 1227, Th/U 0.84, Pb 6; 1.2 U 861, Th 627, Th/U 0.73, Pb 3; 1.3 U 623, Th 212, Th/U 0.34, Pb 71; 2.1 U 867, Th 552, Th/U 0.64, Pb 7; 2.2 U 812, Th 1219, Th/U 1.50, Pb 3; 3.1 U 301, Th 524, Th/U 1.74, Pb 1; 3.2 U 573, Th 230, Th/U 0.40, Pb 72.
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 234 in Records of the Australian Museum 54 (2) on page 234, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15366996
title: Table 9. Summary new whole rock K in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 9. Summary new whole rock K-Ar dating, Tumbarumba-Cabramurra basalts.
sample numberStatusRef.%K#40 Ar*(×10 –10 moles/g)40 Ar*/ 40 Artotalage±1DR14641A11.510.6243308.89423.7±0.2DR13822A20.110.848250.5985397.4±6.7
DR14641 Basanite, Jimmies Road, Granite Mountain (35°43.5'S 148°12.3'E)
DR13822 Olivine micro-dolerite, Ruby Creek (35°49.4' S 148°11.5' E)
Status A: potassium-bearing phases are fresh. Ref. 1—AMDEL laboratories, A. Webb analyst. Ref. 2—CSIRO Division of
Petroleum Research, H. Zwingmann analyst. # mean K value used in age calculations. * denotes radiogenic 40 Ar. Age in Ma with error limits given for the analytical certainly at one standard deviation.
Constants: 40 K = 0.01167 atom%; = 4.962×10 –10 y –1; = 0.581×10 –10 y –1
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 236 in Records of the Australian Museum 54 (2) on page 236, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15366995
title: Table 9. Summary new whole rock K in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 9. Summary new whole rock K-Ar dating, Tumbarumba-Cabramurra basalts.
sample numberStatusRef.%K#40 Ar*(×10 –10 moles/g)40 Ar*/ 40 Artotalage±1DR14641A11.510.6243308.89423.7±0.2DR13822A20.110.848250.5985397.4±6.7
DR14641 Basanite, Jimmies Road, Granite Mountain (35°43.5'S 148°12.3'E)
DR13822 Olivine micro-dolerite, Ruby Creek (35°49.4' S 148°11.5' E)
Status A: potassium-bearing phases are fresh. Ref. 1—AMDEL laboratories, A. Webb analyst. Ref. 2—CSIRO Division of
Petroleum Research, H. Zwingmann analyst. # mean K value used in age calculations. * denotes radiogenic 40 Ar. Age in Ma with error limits given for the analytical certainly at one standard deviation.
Constants: 40 K = 0.01167 atom%; = 4.962×10 –10 y –1; = 0.581×10 –10 y –1
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 236 in Records of the Australian Museum 54 (2) on page 236, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.34740/kaggle/dsv/11736271
title: First Gen Pokemon Classification
DOI: 10.5281/zenodo.15366997
title: Table 10 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 10. Modal mineralogy and melting proportions of mantle types.
mantleOlivineOpxCpxGarnetSpinelKaersutitePhlogopiteSpinel lherzolitemode58.0625.9612.453.53melt prop0.337.6472.9019.13SD0.305.104.850.49Garnet lherzolitemode59.8021.107.6011.50melt prop0.217.5929.6462.56SD0.194.904.301.64Spinelmode59.2724.908.682.145.02amphibolemelt prop1.0814.3617.433.2363.90lherzolite (a)SD1.165.625.872.718.21Garnetmode59.7020.226.469.534.09amphibolemelt prop3.7414.3628.9243.233.74lherzolite (a)SD0.665.620.611.060.66Garnetmode65.6624.233.472.184.47amphibolemelt prop1.596.8613.6824.3753.50lherzolite (b)SD1.062.052.534.663.62Spinelmode58.1825.1812.333.271.05phlogopitemelt prop11.0013.1752.4212.9710.44lherzoliteSD15.5218.5924.983.345.78Garnetmode60.2916.949.785.987.00phlogopitemelt prop1.143.0825.5513.3656.87lherzolite (a)SD0.756.379.6818.9031.05Garnetmode65.3522.365.235.651.42phlogopitemelt prop0.890.8926.1968.333.71lherzolite (b)SD0.580.583.224.894.82
Modal mineralogy of each mantle type is calculated using major element mass balance and also given are the melting proportions (and their standard deviations) which produce the degrees of partial melting listed in Table 11. All values in wt%. All mineral compositions are from McKenzie & O’Nions (1991), except that for amphibole, which is an average value for kaersutite xenocrysts from this study and those used in models GAL (b) and GPL (b), which are from Comin-Chiaramonti et al. (1997). In most models, the bulk mantle composition used is that of the bulk Earth (McKenzie & O’Nions, 1991). The only exceptions are models GAP(b) and GPP(b), which are based on an analysis of a garnet-phlogopite xenolith (Comin-Chiaramonti et al., 1997). Suffix (a) stands for mantle based on the bulk Earth composition given by McKenzie & O’Nions (1991); and (b) for mantle compositions based on a garnet-phlogopite lherzolite from Comin-Chiaramonti et al. (1997).
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 239 in Records of the Australian Museum 54 (2) on page 239, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15366998
title: Table 10 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 10. Modal mineralogy and melting proportions of mantle types.
mantleOlivineOpxCpxGarnetSpinelKaersutitePhlogopiteSpinel lherzolitemode58.0625.9612.453.53melt prop0.337.6472.9019.13SD0.305.104.850.49Garnet lherzolitemode59.8021.107.6011.50melt prop0.217.5929.6462.56SD0.194.904.301.64Spinelmode59.2724.908.682.145.02amphibolemelt prop1.0814.3617.433.2363.90lherzolite (a)SD1.165.625.872.718.21Garnetmode59.7020.226.469.534.09amphibolemelt prop3.7414.3628.9243.233.74lherzolite (a)SD0.665.620.611.060.66Garnetmode65.6624.233.472.184.47amphibolemelt prop1.596.8613.6824.3753.50lherzolite (b)SD1.062.052.534.663.62Spinelmode58.1825.1812.333.271.05phlogopitemelt prop11.0013.1752.4212.9710.44lherzoliteSD15.5218.5924.983.345.78Garnetmode60.2916.949.785.987.00phlogopitemelt prop1.143.0825.5513.3656.87lherzolite (a)SD0.756.379.6818.9031.05Garnetmode65.3522.365.235.651.42phlogopitemelt prop0.890.8926.1968.333.71lherzolite (b)SD0.580.583.224.894.82
Modal mineralogy of each mantle type is calculated using major element mass balance and also given are the melting proportions (and their standard deviations) which produce the degrees of partial melting listed in Table 11. All values in wt%. All mineral compositions are from McKenzie & O’Nions (1991), except that for amphibole, which is an average value for kaersutite xenocrysts from this study and those used in models GAL (b) and GPL (b), which are from Comin-Chiaramonti et al. (1997). In most models, the bulk mantle composition used is that of the bulk Earth (McKenzie & O’Nions, 1991). The only exceptions are models GAP(b) and GPP(b), which are based on an analysis of a garnet-phlogopite xenolith (Comin-Chiaramonti et al., 1997). Suffix (a) stands for mantle based on the bulk Earth composition given by McKenzie & O’Nions (1991); and (b) for mantle compositions based on a garnet-phlogopite lherzolite from Comin-Chiaramonti et al. (1997).
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 239 in Records of the Australian Museum 54 (2) on page 239, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15367000
title: Table 11 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 11. Degrees of partial melting for Tumbarumba primary magma compositions.
samplegarnet lherzolitegarnet-amphibole lherzolitegarnet-amphibole lherzolitegarnet-phlogopite lherzolitegarnet-phlogopite lherzolitespinel lherzolitespinelamphibole lherzolite(a)(b)(a)(b)146396.603.004.202.817.798.136.82138355.102.991.976.275.926.746.12146505.600.501.955.457.28138205.571.552.723.855.047.10146625.301.162.865.586.946.34138285.491.854.624.976.667.019.59146414.651.211.714.055.876.237.791594.861.802.294.606.236.49616.021.244.734.136.357.463.95634.502.141.413.538.146.04averagesbasanite alkali basalt5.371.442.664.575.706.966.05basalt5.532.333.413.777.537.068.21olivine basalt4.861.802.294.606.236.49average basalt5.362.203.133.987.206.92
14639 alkali basalt, 13835 basanite, 14650 basanite, 13820 basanite, 14662 basanite, 13828 alkali basalt, 14641 basanite, 159
olivine basalt, 61 basanite, 63 alkali olivine basalt.
Degrees of partial melting are calculated by major element mass balance (see Table 10). All values in wt%.
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 239 in Records of the Australian Museum 54 (2) on page 239, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15366999
title: Table 11 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 11. Degrees of partial melting for Tumbarumba primary magma compositions.
samplegarnet lherzolitegarnet-amphibole lherzolitegarnet-amphibole lherzolitegarnet-phlogopite lherzolitegarnet-phlogopite lherzolitespinel lherzolitespinelamphibole lherzolite(a)(b)(a)(b)146396.603.004.202.817.798.136.82138355.102.991.976.275.926.746.12146505.600.501.955.457.28138205.571.552.723.855.047.10146625.301.162.865.586.946.34138285.491.854.624.976.667.019.59146414.651.211.714.055.876.237.791594.861.802.294.606.236.49616.021.244.734.136.357.463.95634.502.141.413.538.146.04averagesbasanite alkali basalt5.371.442.664.575.706.966.05basalt5.532.333.413.777.537.068.21olivine basalt4.861.802.294.606.236.49average basalt5.362.203.133.987.206.92
14639 alkali basalt, 13835 basanite, 14650 basanite, 13820 basanite, 14662 basanite, 13828 alkali basalt, 14641 basanite, 159
olivine basalt, 61 basanite, 63 alkali olivine basalt.
Degrees of partial melting are calculated by major element mass balance (see Table 10). All values in wt%.
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 239 in Records of the Australian Museum 54 (2) on page 239, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15367001
title: Table 12 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 12. Comparative key mantle-normalised incompatible element ranges, selected primary Na-rich basalts, eastern Australian sapphire fields.
basalt field no. analysesSnowyaBarringtonb OberoncNew Englandd Hoy, Qlde NE Tasf6107331SiO243.1–46.241.4–46.543.2–45.744.0–44.742.0–44.944.6MgO9.3–16.89.0–12.38.8–12.98.0–9.59.6–12.48.7Ka2O/Na2O0.24–0.470.19–0.370.20–0.450.45–0.480.39–0.490.31KN23–5425–5329–5433–5440–5726PN25–6524–6217–3227–6527–6519ZrN10–1710–2114–2713–2415–2114NbN80–19052–13256–12259–9859–12659RbN16–4816–5022–4633–3630–5025ThN59–14135–18824–7124–9430TaN122–22049–195
a this paper (4Bsn, 2AOB). b O’Reilly & Zhang (1995) and Sutherland & Fanning (2001) (3 Ne, 5Bsn, 2AOB). c Morris (1986) (5Bsn, 2AOB). d Coenraads (1994) (3AOB). e Sutherland & Robertson (unpublished data) (1Ne, 2AOB). f Sutherland et al. (1989) (1AOB). primitive mantle normalised values, based on Sun N & McDonough (1989). Ne, Nephelinite; Bsn, Basanite; AOB, Alkali Olivine Basalt.
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 243 in Records of the Australian Museum 54 (2) on page 243, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.5281/zenodo.15367002
title: Table 12 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia

description: Table 12. Comparative key mantle-normalised incompatible element ranges, selected primary Na-rich basalts, eastern Australian sapphire fields.
basalt field no. analysesSnowyaBarringtonb OberoncNew Englandd Hoy, Qlde NE Tasf6107331SiO243.1–46.241.4–46.543.2–45.744.0–44.742.0–44.944.6MgO9.3–16.89.0–12.38.8–12.98.0–9.59.6–12.48.7Ka2O/Na2O0.24–0.470.19–0.370.20–0.450.45–0.480.39–0.490.31KN23–5425–5329–5433–5440–5726PN25–6524–6217–3227–6527–6519ZrN10–1710–2114–2713–2415–2114NbN80–19052–13256–12259–9859–12659RbN16–4816–5022–4633–3630–5025ThN59–14135–18824–7124–9430TaN122–22049–195
a this paper (4Bsn, 2AOB). b O’Reilly & Zhang (1995) and Sutherland & Fanning (2001) (3 Ne, 5Bsn, 2AOB). c Morris (1986) (5Bsn, 2AOB). d Coenraads (1994) (3AOB). e Sutherland & Robertson (unpublished data) (1Ne, 2AOB). f Sutherland et al. (1989) (1AOB). primitive mantle normalised values, based on Sun N & McDonough (1989). Ne, Nephelinite; Bsn, Basanite; AOB, Alkali Olivine Basalt.
description: Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 243 in Records of the Australian Museum 54 (2) on page 243, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489
DOI: 10.21233/7er0-ba98
title: Le Stade pollen dataset

description: Raw data for the Le Stade pollen dataset submitted to the Neotoma Paleoecology Database. Data is available through the landing page in JSON format. The landing page referenced by the DOI also contains links to publications and a map-based viewer for the dataset. The Neotoma Paleoecology Database maintains a homepage at https://www.neotomadb.org.
DOI: 10.15468/dl.sx9c5h
title: Occurrence Download

description: A dataset containing 3 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Oreopteris quelpaertensis (Christ) Holub",
 "Year is greater than or equal to 1980",
 "Year is less than or equal to 2010",
 "HasCoordinate is true"
 ]
}

 The dataset includes 3 records from 2 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0022030-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.21233/taad-rc48
title: LDDsite4834 water chemistry dataset

description: Raw data for the LDDsite4834 water chemistry dataset submitted to the Neotoma Paleoecology Database. Data is available through the landing page in JSON format. The landing page referenced by the DOI also contains links to publications and a map-based viewer for the dataset. The Neotoma Paleoecology Database maintains a homepage at https://www.neotomadb.org.