IntChron > doi > 10.1016 > j.quascirev.2003.11.006
labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
QUEST420/121/01 | QUEST-20 | QUEST-WDS | 73.86 | 0.3 | 11.93 | 2.53 | 0.08 | 0.25 | 1.54 | 3.32 | 2.45 | 0 | 0 | 0 | 96.27 | 1 | ||
QUEST420/121/02 | QUEST-20 | QUEST-WDS | 72.93 | 0.33 | 11.76 | 2.5 | 0.07 | 0.27 | 1.57 | 3.44 | 2.48 | 0 | 0 | 0 | 95.35 | 1 | ||
QUEST420/121/03 | QUEST-20 | QUEST-WDS | 74.04 | 0.31 | 11.88 | 2.45 | 0.09 | 0.27 | 1.65 | 3.2 | 2.47 | 0 | 0 | 0 | 96.36 | 1 | ||
QUEST420/121/04 | QUEST-20 | QUEST-WDS | 75.01 | 0.29 | 12.03 | 2.55 | 0.09 | 0.26 | 1.57 | 2.89 | 2.55 | 0 | 0 | 0 | 97.24 | 1 | ||
QUEST420/121/05 | QUEST-20 | QUEST-WDS | 75.05 | 0.31 | 12.23 | 2.54 | 0.08 | 0.25 | 1.63 | 3.08 | 2.51 | 0 | 0 | 0 | 97.67 | 1 |
labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
QUEST420/122/01 | QUEST-20 | QUEST-WDS | 74.22 | 0.07 | 11.8 | 1.21 | 0.02 | 0.03 | 0.52 | 3.49 | 3.96 | 0 | 0 | 0 | 95.31 | 1 | ||
QUEST420/122/02 | QUEST-20 | QUEST-WDS | 74.86 | 0.11 | 11.63 | 1.05 | 0.02 | 0.04 | 0.39 | 3.12 | 4.04 | 0 | 0 | 0 | 95.26 | 1 | ||
QUEST420/122/03 | QUEST-20 | QUEST-WDS | 74.73 | 0.09 | 11.6 | 0.96 | 0.03 | 0.04 | 0.4 | 3.04 | 4.26 | 0 | 0 | 0 | 95.15 | 1 | ||
QUEST420/122/04 | QUEST-20 | QUEST-WDS | 74.23 | 0.11 | 11.6 | 1.11 | 0.05 | 0.05 | 0.46 | 3.2 | 3.7 | 0 | 0 | 0 | 94.51 | 1 | ||
QUEST420/122/05 | QUEST-20 | QUEST-WDS | 73.95 | 0.11 | 11.79 | 1.13 | 0.01 | 0.06 | 0.47 | 3.12 | 4.06 | 0 | 0 | 0 | 94.7 | 1 | ||
QUEST420/122/06 | QUEST-20 | QUEST-WDS | 73.8 | 0.11 | 11.8 | 1.16 | 0.03 | 0.05 | 0.47 | 3.24 | 3.83 | 0 | 0 | 0 | 94.5 | 1 | ||
QUEST420/122/07 | QUEST-20 | QUEST-WDS | 74.39 | 0.1 | 11.62 | 0.98 | 0.01 | 0.01 | 0.43 | 2.77 | 4.07 | 0 | 0 | 0 | 94.38 | 1 | ||
QUEST420/122/08 | QUEST-20 | QUEST-WDS | 73.48 | 0.1 | 11.77 | 1.29 | 0.05 | 0.02 | 0.54 | 3.22 | 3.74 | 0 | 0 | 0 | 94.22 | 1 | ||
QUEST420/122/09 | QUEST-20 | QUEST-WDS | 73.51 | 0.09 | 11.84 | 1.21 | 0.03 | 0.02 | 0.55 | 3.24 | 3.67 | 0 | 0 | 0 | 94.16 | 1 | ||
QUEST420/122/10 | QUEST-20 | QUEST-WDS | 73.32 | 0.08 | 11.74 | 1.12 | 0.05 | 0.03 | 0.5 | 3.39 | 3.97 | 0 | 0 | 0 | 94.18 | 1 |
labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
QUEST420/136/01 | QUEST-20 | QUEST-WDS | 73.57 | 0.14 | 12.39 | 1.47 | 0.04 | 0.04 | 0.72 | 3.39 | 3.99 | 0 | 0 | 0 | 95.75 | 1 | ||
QUEST420/136/02 | QUEST-20 | QUEST-WDS | 73.11 | 0.13 | 12.3 | 1.52 | 0 | 0.07 | 0.77 | 3.62 | 3.68 | 0 | 0 | 0 | 95.2 | 1 | ||
QUEST420/136/03 | QUEST-20 | QUEST-WDS | 73.02 | 0.14 | 12.38 | 1.59 | 0.05 | 0.07 | 0.66 | 3.47 | 3.8 | 0 | 0 | 0 | 95.18 | 1 | ||
QUEST420/136/04 | QUEST-20 | QUEST-WDS | 72.9 | 0.14 | 12.3 | 1.5 | 0.04 | 0.09 | 0.72 | 3.37 | 3.9 | 0 | 0 | 0 | 94.96 | 1 | ||
QUEST420/136/05 | QUEST-20 | QUEST-WDS | 73.18 | 0.07 | 12.27 | 1.5 | 0.03 | 0.09 | 0.77 | 3.26 | 3.76 | 0 | 0 | 0 | 94.93 | 1 | ||
QUEST420/136/06 | QUEST-20 | QUEST-WDS | 72.99 | 0.14 | 12.36 | 1.51 | 0.02 | 0.09 | 0.79 | 3.38 | 3.63 | 0 | 0 | 0 | 94.91 | 1 | ||
QUEST420/136/07 | QUEST-20 | QUEST-WDS | 73.12 | 0.1 | 12.23 | 1.57 | 0.03 | 0.09 | 0.72 | 3.25 | 3.72 | 0 | 0 | 0 | 94.83 | 1 | ||
QUEST420/136/08 | QUEST-20 | QUEST-WDS | 72.87 | 0.11 | 12.47 | 1.51 | 0.05 | 0.08 | 0.74 | 3.29 | 3.69 | 0 | 0 | 0 | 94.81 | 1 | ||
QUEST420/136/09 | QUEST-20 | QUEST-WDS | 72.64 | 0.13 | 12.28 | 1.61 | 0 | 0.11 | 0.83 | 3.53 | 3.68 | 0 | 0 | 0 | 94.81 | 1 | ||
QUEST420/136/10 | QUEST-20 | QUEST-WDS | 73.12 | 0.1 | 12.19 | 1.4 | 0.07 | 0.06 | 0.68 | 3.31 | 3.83 | 0 | 0 | 0 | 94.75 | 1 | ||
QUEST420/136/11 | QUEST-20 | QUEST-WDS | 72.93 | 0.13 | 12.22 | 1.53 | 0.06 | 0.08 | 0.74 | 3.37 | 3.68 | 0 | 0 | 0 | 94.74 | 1 | ||
QUEST420/136/12 | QUEST-20 | QUEST-WDS | 72.76 | 0.18 | 12.18 | 1.5 | 0.03 | 0.1 | 0.77 | 3.36 | 3.86 | 0 | 0 | 0 | 94.74 | 1 | ||
QUEST420/136/13 | QUEST-20 | QUEST-WDS | 72.72 | 0.11 | 11.98 | 1.5 | 0.06 | 0.1 | 0.74 | 3.66 | 3.87 | 0 | 0 | 0 | 94.74 | 1 | ||
QUEST420/136/14 | QUEST-20 | QUEST-WDS | 72.91 | 0.12 | 12.09 | 1.35 | 0.05 | 0.05 | 0.83 | 3.38 | 3.92 | 0 | 0 | 0 | 94.7 | 1 | ||
QUEST420/136/15 | QUEST-20 | QUEST-WDS | 72.86 | 0.13 | 12.29 | 1.49 | 0.05 | 0.05 | 0.77 | 3.36 | 3.69 | 0 | 0 | 0 | 94.69 | 1 | ||
QUEST420/136/16 | QUEST-20 | QUEST-WDS | 72.77 | 0.11 | 12.29 | 1.51 | 0.07 | 0.12 | 0.74 | 3.41 | 3.66 | 0 | 0 | 0 | 94.68 | 1 | ||
QUEST420/136/17 | QUEST-20 | QUEST-WDS | 72.6 | 0.13 | 12.34 | 1.47 | 0.06 | 0.07 | 0.84 | 3.46 | 3.68 | 0 | 0 | 0 | 94.63 | 1 | ||
QUEST420/136/18 | QUEST-20 | QUEST-WDS | 73.03 | 0.11 | 12.24 | 1.48 | 0.05 | 0.06 | 0.76 | 3.3 | 3.57 | 0 | 0 | 0 | 94.58 | 1 | ||
QUEST420/136/19 | QUEST-20 | QUEST-WDS | 72.69 | 0.17 | 12.12 | 1.5 | 0 | 0.11 | 0.9 | 3.38 | 3.67 | 0 | 0 | 0 | 94.54 | 1 | ||
QUEST420/136/20 | QUEST-20 | QUEST-WDS | 72.98 | 0.16 | 12.39 | 1.18 | 0.04 | 0.08 | 0.62 | 3.4 | 3.67 | 0 | 0 | 0 | 94.52 | 1 | ||
QUEST420/136/21 | QUEST-20 | QUEST-WDS | 73.08 | 0.11 | 12.25 | 1.09 | 0.02 | 0.03 | 0.7 | 3.31 | 3.78 | 0 | 0 | 0 | 94.37 | 1 | ||
QUEST420/136/22 | QUEST-20 | QUEST-WDS | 72.61 | 0.13 | 12.27 | 1.48 | 0.05 | 0.08 | 0.76 | 3.24 | 3.74 | 0 | 0 | 0 | 94.34 | 1 | ||
QUEST420/136/23 | QUEST-20 | QUEST-WDS | 72.34 | 0.13 | 12.32 | 1.49 | 0.02 | 0.09 | 0.7 | 3.23 | 3.82 | 0 | 0 | 0 | 94.14 | 1 |
z | z_range | t | t_sigma | sample | volc_region | volcano | eruption | ref | ||
---|---|---|---|---|---|---|---|---|---|---|
-8859.5 | 240 | QUEST420/121 | NVZ | Askja | Askja-S | doi:10.1016/s0033-5894(03)00035-8 | ||||
-9437.5 | 156 | QUEST420/122 | SVB | Snaefellsjokull | Hasseldalen tephra | doi:10.1016/s0033-5894(03)00035-8 |
eruption | eruption_type | t | t_sigma | t_source | ref | notes | ||
---|---|---|---|---|---|---|---|---|
PMG-5 | Plinian | 1600.5 | 100 | doi:10.1191/0959683602hl538rr | possibly c. AD 1600 interpolated (Hall & Pilcher 2002). | |||
BIP-24 | Plinian | 900.5 | 100 | doi:10.1111/j.1502-3885.2005.tb01011.x | c. AD 900 interpolated | |||
AD860 Layer part B | Plinian | 860.5 | 20 | doi:10.1177/095968369500500111 | c. AD 860 ± 20 radiocarbon wiggle-match at Sluggan (AD lower layer, colourless tephra shards, two populations) | |||
OMH-185 (Barnsmore) | Plinian | -716.5 | 38 | IntCal04 | doi:10.1191/0959683604hl757rr | c. 755-680 cal BC (Plunkett et al. 2004). According to Hall and Pilcher (2002) this is probably equivalent to the DOM-6 'microlite' tephra in Germany. | ||
Derrycunihy Wood SH-1 | Plinian | |||||||
FMAZ II (Fugloyarbanki) | Plinian | -24739.5 | 1 | GICC05 | doi:10.1002/jqs.1182 | 26740 ± 390 yr b2k in NGRIP 1848.05 | ||
Borrobol | Plinian | -12094.5 | 95 | IntCal09 | doi:10.1002/jqs.1498 | Best current estimate is 14.14-13.95 cal ka BP (Bayesian age model). Replaces Turney et al. (1997) date of c.14.4 cal ka BP. Davies et al. (2004) suggestion of 2 eruptions has been revised by Matthews et al. (2011). | ||
L3574 | Plinian | No age given, reported as 'older than Saksunarvatn tephra' by Dugmore and Newton (1997). Turney et al. (2006) suggests an age of c. 10.8 ka cal. BP. | ||||||
OWB-105 AD700 | Plinian | 700.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 700 interpolated (Hall & Pilcher 2002). | |||
Penifiler Tephra | Plinian | -11929.5 | 200 | IntCal09 | doi:10.1002/jqs.1498 | 14.08-13.68 cal ka BP (Bayesian age model) | ||
Sluggan A | Plinian | -12549.5 | 500 | doi:10.1002/jqs.990 | c. 14500 cal BP suggested by Turney et al. (2006) | |||
Sluggan B | Plinian | -10849.5 | 500 | doi:10.1002/jqs.990 | c. 12800 cal BP suggested by Turney et al. (2006) | |||
AD860 Layer part A | Plinian | 860.5 | 20 | doi:10.1177/095968369500500111 | c. AD 860 ± 20 radiocarbon wiggle-match at Sluggan (AD lower layer, colourless tephra shards, two populations) | |||
BMR-90 AD920 | Plinian | 920.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 920 interpolated (Hall & Pilcher 2002) | |||
Breakish Tephra | Plinian | doi:10.1002/jqs.1066 | no date suggested although position above the Ashik tephra and Saksunarvatn indicates an age in the early-mid Holocene. | |||||
DOM-6 'microlite' tephra | Plinian | -696.5 | 35 | doi:10.1006/qres.2002.2325 | c. 730-664 cal BC radiocarbon (van den Bogaard et al. 2002). According to Hall & Pilcher (2002) this is probably equivalent to the OMH-185 (Barnsmore) tephra. | |||
GB4-182 | Plinian | -1349.5 | 200 | doi:10.1191/0959683602hl538rr | c. 1350 cal BC interpolated (Hall & Pilcher 2002) | |||
GB4-50 AD1250 | Plinian | 1250.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 1250 interpolated (Hall & Pilcher 2002) | |||
Harthorpe Moss tephra | Plinian | doi:10.1177/095968369600600112 | ||||||
Lough Portain B | Plinian | 0 | doi:10.1177/095968369500500301 | sub-population of Hekla AD 1510 eruption (Lough Portain A). Status is unclear, not a distinct isochrone | ||||
MOR-T4 | Plinian | 1000.5 | 100 | doi:10.1191/0959683604hl749rp | c. cal AD 1000 interpolated (Chambers et al. 2004) | |||
Roddans Port A | Plinian | doi:10.1002/jqs.990 | two sub-populations (A & B) at 63-64 cm depth, dating unclear, pre-Vedde Ash. | |||||
Roddans Port B | Plinian | doi:10.1002/jqs.990 | two sub-populations (A & B) at 63-64 cm depth, dating unclear, pre-Vedde Ash. | |||||
SLU-5 | Plinian | 1650.5 | 50 | doi:10.1191/0959683602hl538rr | c. AD 1600-1700 interpolated (Hall & Pilcher 2002) | |||
Stomyren tephra | Plinian | -149.5 | 100 | doi:10.1016/j.quaint.2004.04.030 | c. 2100 cal yr BP interpolated (Wastegard 2005) | |||
Vallensgard Mose tephra | Plinian | doi:10.1002/jqs.990 | Stratigraphic position is similar to Vedde Ash, in the middle of the Younger Dryas, but geochemistry is different. Unclear if this is a significant tephra horizon. | |||||
NAAZ I | Plinian | -10449.5 | 500 | Marine04 | doi:10.1016/j.quascirev.2006.03.001 | Diffuse layer representing c. 11 ka 14C yr GS-1 ash zone containing components from I-Thol-2 (Grímsvötn), I-Rhy.1 (Katla) and I-Thol-1 (Veidivötn). It is commonly believed that the biggest contributor is the rhyolitic component of the Vedde Ash. | ||
L-274 | Plinian | -8274.5 | 100 | IntCal09 | doi:10.1016/j.quaint.2011.05.014 | 14C modeled age of 10,325-10,125 yr cal BP (Lind & Wastegard 2011). | ||
5d-BAS | Plinian | -109549.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably represents an eruption complex. Several geochemical populations: BAS-I, BAS-II, BAS-III. | ||
5e-Midt | Plinian | -123049.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably represents an eruption complex. Several geochemical populations: RHY, INT, BAS & TAB (the 5e-Midt/TRACHY is believed to be from Jan Mayen). Wallrabe-Adams & Lackschewitz (2002) suggest either Vatnafjoll or Vestmannaeyjar may be the source. | ||
5e-Low | Plinian | -127549.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably represents an eruption complex. Several geochemical populations. Wallrabe-Adams & Lackschewitz (2002) suggest either Vatnafjoll or Vestmannaeyjar may be the source. | ||
St. 5a-THOL-1 | Plinian | -74549.5 | 5000 | Orbital | doi:10.1016/0012-821x(95)00145-3 | THOL geochemical composition | ||
St. 7-RHY-I & II | Plinian | -208049.5 | 20000 | Orbital | doi:10.1002/jqs.3390060205 | RHY-I & RHY-II geochemical compositions | ||
St. 7-BAS/INT-I | Plinian | -208549.5 | 20000 | Orbital | doi:10.1002/jqs.3390060205 | INT-I & INT/BAS-I geochemical compositions | ||
St. 9-RHY-I | Plinian | -328049.5 | 30000 | Orbital | doi:10.1002/jqs.3390060205 | RHY geochemical composition; possible equivalent to NAAZ III (III-RHY-I, c.320 ka) | ||
St. 9-BAS-I | Plinian | -328049.5 | 30000 | Orbital | doi:10.1002/jqs.3390060205 | BAS geochemcial composition |
site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Ballysculllian East | UK | -6.462999821 | 54.79750061 | 44 | Terrestrial | QUEST621/111 | distal | fall | ash | quest | |||||
Borg Indrepollen | Norway | 13.49400043 | 68.14499664 | Terrestrial | QUEST636/111 | distal | fall | ash | quest |
site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Borg Indrepollen | Norway | 13.49400043 | 68.14499664 | Terrestrial | QUEST636/110 | distal | fall | ash | quest |
site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Derrycunihy Wood | Ireland | -9.416669846 | 52.01670074 | Terrestrial | QUEST580/113 | distal | fall | ash | quest |
site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
K708-1 | -23.75 | 50 | -4053 | Marine | QUEST709/3 | distal | fall | ash | quest |