cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.26342023
title: <b>Data for Needs assessment for Master of Nursing program among Kenyan Nurses</b>

description: <b>Abstract</b><b>Background</b>Nurses comprise the dominant cadre of healthcare workers yet there remains an acute shortage of nurses globally with Africa most affected. However, access to higher nursing education in sub-Saharan Africa remains limited. We aimed to i) Assess the need for a Master of Nursing (MScN) program among graduate nurses in Kenya ii) Identify preferred MScN program options among graduate nurses intending to enrol for MScN in Kenya iii) Identify skills mismatch among graduate nurses in Kenya iv) Assess the relationship between intention to enrol in MScN program and job satisfaction among graduate nurses in Kenya.<b>Methods</b>A cross-sectional design employing an online survey was used. Consenting nurses with a first degree in general nursing or any of the nursing speciality areas were included. Socio-demographic data were collected using a questionnaire. The ward organizational features scale was used to assess job satisfaction. The Program for the International Assessment of Adult Competencies background questionnaire was used to assess skills mismatch. The need for an MScN program was assessed by determining the proportion of participants who expressed the intention to join the MScN program. Preferred MScN program options were determined as frequencies and proportions. Skills mismatch was computed as frequencies and proportions. The relationship between the need for MScN and job satisfaction was assessed using the point biserial-correlation.<b>Results</b>A total of 420 volunteers were screened out of which 355 were enrolled. Overall, 337 (94.9% [95% CI: 92.1 – 96.9]) of volunteers expressed the desire to pursue MScN training. Among volunteers who expressed desire to pursue an MScN, majority preferred to study the critical care/renal specialty (24.9% [95% CI: 20.3 – 29.9]). A majority of the volunteers (319 [89.9%]) felt their skills were inferior to their responsibilities (under skilled). We found no significant correlation between the need for MScN and job satisfaction (r = 0.058; p = 0.269).<b>Conclusion</b>Our findings suggest a strong desire by graduate nurses in Kenya to pursue MScN with a preference for critical care specialization while part-time is the preferred learning mode. Additionally, most nurses felt their skills were inferior to their professional responsibilities. There was no correlation between the intention to pursue MScN and job satisfaction. There is a need to establish more MScN programs in Kenya coupled with the deployment of nurses as per the scope of practice.
DOI: 10.6084/m9.figshare.26342023.v1
title: <b>Data for Needs assessment for Master of Nursing program among Kenyan Nurses</b>

description: <b>Abstract</b><b>Background</b>Nurses comprise the dominant cadre of healthcare workers yet there remains an acute shortage of nurses globally with Africa most affected. However, access to higher nursing education in sub-Saharan Africa remains limited. We aimed to i) Assess the need for a Master of Nursing (MScN) program among graduate nurses in Kenya ii) Identify preferred MScN program options among graduate nurses intending to enrol for MScN in Kenya iii) Identify skills mismatch among graduate nurses in Kenya iv) Assess the relationship between intention to enrol in MScN program and job satisfaction among graduate nurses in Kenya.<b>Methods</b>A cross-sectional design employing an online survey was used. Consenting nurses with a first degree in general nursing or any of the nursing speciality areas were included. Socio-demographic data were collected using a questionnaire. The ward organizational features scale was used to assess job satisfaction. The Program for the International Assessment of Adult Competencies background questionnaire was used to assess skills mismatch. The need for an MScN program was assessed by determining the proportion of participants who expressed the intention to join the MScN program. Preferred MScN program options were determined as frequencies and proportions. Skills mismatch was computed as frequencies and proportions. The relationship between the need for MScN and job satisfaction was assessed using the point biserial-correlation.<b>Results</b>A total of 420 volunteers were screened out of which 355 were enrolled. Overall, 337 (94.9% [95% CI: 92.1 – 96.9]) of volunteers expressed the desire to pursue MScN training. Among volunteers who expressed desire to pursue an MScN, majority preferred to study the critical care/renal specialty (24.9% [95% CI: 20.3 – 29.9]). A majority of the volunteers (319 [89.9%]) felt their skills were inferior to their responsibilities (under skilled). We found no significant correlation between the need for MScN and job satisfaction (r = 0.058; p = 0.269).<b>Conclusion</b>Our findings suggest a strong desire by graduate nurses in Kenya to pursue MScN with a preference for critical care specialization while part-time is the preferred learning mode. Additionally, most nurses felt their skills were inferior to their professional responsibilities. There was no correlation between the intention to pursue MScN and job satisfaction. There is a need to establish more MScN programs in Kenya coupled with the deployment of nurses as per the scope of practice.
DOI: 10.1594/pangaea.722658
title: Other measurements at 10 m from station Rock Springs (2004-10)
DOI: 10.1594/pangaea.723142
title: Oxygen isotope ratios amd Li concentrations in spilitized basaltic rocks of DSDP Hole 83-504B (Table 5)

description: Li-delta18O-SiO2 relationships have been examined for suites of spilitized basaltic rocks (DSDP 504B; Xigaze Ophiolite; Blanco Fracture Zone; Greater Caucasus; Rhenohercynian Fold Belt) and intra-plate evolved tholeiites (Northern Hessian Depression and Vogelsberg, W Germany; Mount Falla, Transantarctic Mountains). Relative to unaltered MORB and intra-plate primary olivine tholeiites, both the spilitic rocks and the evolved tholeiites are characterized by Li and 18O enrichment. For the spilitic rocks, Li and 18O enrichment is accompanied by a loss of SiO2 as a result of seawater hydrothermal alteration, whereas the evolved tholeiites have gained SiO2, Li and 18O from fractionation of mafic phases and assimilation of crustal rocks.On Li vs. SiO2 and delta18O vs. SiO2 diagrams, the two rock groups plot largely in distinct fields, suggesting the possibility of so distinguishing between such lithologies in the ancient rock record. Mafic granulite xenoliths from the Northern Hessian Depression have elevated Li and 18O abundances at low SiO2 contents. Even after correction for extraction of felsic components, their Li-delta18O-SiO2 signatures plot within the field of spilitic protoliths, suggesting that the lower crust in this region contains relics of spilitic rocks from a former oceanic crust.
description: For SiO2 data see Emmermann (1985) dataset: doi:10.1594/PANGAEA.262215
description: Supplement to: Mengel, K; Hoefs, Jochen (1990): Li-d18O-SiO2 systematics in volcanic rocks and mafic lower crustal granulite xenoliths. Earth and Planetary Science Letters, 101(1), 42-53
DOI: 10.1594/pangaea.722951
title: Ultra-violet measurements from station Rock Springs (2000-12)

description: Version 2, 2009-06-26. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.930074
title: Macroscopic charcoal counts and areas from sediment core Ghats_MY

description: Analyst: Walter Finsinger
DOI: 10.1594/pangaea.687228
title: Total organic carbon from bottle APRIL-2000-K1

description: The samples (10 ml) were obtained in pre-combusted (480oC, 12 h) glass ampoules, acidified with HCl to 0.1% by volume and flame - sealed immediately on board. High Temperature Catalytic Oxidation HTCO using a Shimadzu 5000 TOC analyzer. Sugimura, Y & Y. Suzuki, 1988. Cauwet, G., 1994.
DOI: 10.1594/pangaea.722956
title: Ultra-violet measurements from station Rock Springs (2001-01)

description: Version 2, 2009-06-26. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.722963
title: Other measurements at 10 m from station Rock Springs (2001-03)

description: Version 2, 2009-06-26
DOI: 10.1594/pangaea.723359
title: Description of profile 7441-102
DOI: 10.1594/pangaea.722965
title: Ultra-violet measurements from station Rock Springs (2001-04)

description: Version 2, 2009-06-26. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.722974
title: Ultra-violet measurements from station Rock Springs (2001-07)

description: Version 2, 2009-06-26. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.723692
title: Radiosonde measurements from station Southern Great Plains (2003-10)

description: Version 2, 2009-07-02; Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.773926
title: (Table T1) CaCO3 content in ODP Hole 167-1012A
DOI: 10.1594/pangaea.722975
title: Other measurements at 10 m from station Rock Springs (2001-07)

description: Version 2, 2009-06-26
DOI: 10.1594/pangaea.723360
title: Description of profile 7441-103
DOI: 10.1594/pangaea.723373
title: Basic measurements of radiation at station Billings (1993-11)

description: Version 2, 2009-07-02
DOI: 10.1594/pangaea.887599
title: Basic measurements of radiation at station Gandhinagar (2014-09)

description: Short-wave nighttime values were artificially set to 0, this will be changed in February 2019.
DOI: 10.1594/pangaea.723532
title: Radiosonde measurements from station Southern Great Plains (1998-10)

description: Version 2, 2009-07-02; Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.694683
title: Yearly production of marine products and its process lines in Region II, Chile, 1998
DOI: 10.1594/pangaea.722853
title: Ultra-violet measurements from station Rock Springs (1998-08)

description: Version 2, 2009-06-26. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.722721
title: Ultra-violet measurements from station Rock Springs (2006-04)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.872085
title: Particle fluxes from time series station Iwik
DOI: 10.1594/pangaea.930069
title: Age determination of sediment core Ghats_MY

description: Most radiocarbon dates were published in Bhagwat et al., 2012; 2014.
DOI: 10.1594/pangaea.720136
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 15-154

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.723636
title: Basic measurements of radiation at station Billings (2002-03)

description: Version 2, 2009-07-02
DOI: 10.1594/pangaea.720143
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 21-203

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.722059
title: Ultra-violet measurements from station Goodwin Creek (2007-08)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.720153
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 58-444A

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.720157
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 58-446

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.722877
title: Ultra-violet measurements from station Rock Springs (1999-03)

description: Version 2, 2009-06-26. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.722074
title: Ultra-violet measurements from station Goodwin Creek (2008-01)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.687225
title: Particulate organic carbon and nitrogen from bottle APRIL-2000-K4

description: POC/PON measured on a EA 1108 CHN Fisons Instruments CHN analyser according to the methodology suggested by Cutter, G.A. & J. Radford-Knoery (1991) and Verardo et al (1990).
DOI: 10.1594/pangaea.720160
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 59-450

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.722931
title: Other measurements at 10 m from station Rock Springs (2000-05)

description: Version 2, 2009-06-26