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Text Description: Quartz gabbro from elevation 1,000 feet on the west-facing hill slope 2 3/4 miles southwest of Tarasof Point. The texture is hypidiomorphic-granular. Felsic minerals compose 75-80 percent of the rock: 4-6 percent quartz, <0.1 percent orthoclase, and 70-75 percent plagioclase slightly altered to sericite (<0.1 percent). The plagioclase composition, by extinction angle, is An54 [mean of 36 crystals, standard deviation is 7 percent An, average amount of zoning per individual plagioclase crystal is 9 percent An per crystal]. Mafic minerals compose 20-25 percent: 0.5-1.5 percent clinopyroxene (remnants in hornblende and euhedra in feldspar), 8-10 percent hornblende (an indeterminate amount derived from clinopyroxene), 6-8 percent biotite slightly altered to penninite (<0.1 percent) and cliozoisite (<0.1 percent), 2-5 percent magnetite, <0.1 percent hematite, 0.5-1.5 percent apatite, 0.5-1 percent tourmaline, and 0.1-1 percent penninite (interstitial). References: ![]() |
StationID | Latitude | Longitude | Geologist | DateVisited | Age Info | Volcano | Eruption | Location Description | Text Description | Sample ID | Sample Type 1 | Sample Type 2 | Final Unit | Material | SiO2 | TiO2 | Al2O3 | FeOT | MnO | MgO | CaO | Na2O | K2O | P2O5 | Total-majors | REF majors | METH majors | Fe2O3/Fe203T orig | FeO/FeOT orig | Volatiles csv | METH volatiles | Cs | Rb | Ba | Sr | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Y | Zr | Nb | Hf | Ta | Pb | Th | U | Sc | V | Cr | Fe | Co | Ni | Cu | Zn | Ga | Mo | As | Na | K | Ref trace1 | METH trace1 | Rb | Ba | Sr | La | Ce | Nd | Sm | Eu | Gd | Dy | Er | Yb | Lu | Y | Zr | Nb | Pb | Th | U | Sc | Ti | V | Cr | Ni | Cu | Zn | Ga | Ref trace2 | METH trace2 | Light csv | Halogen csv | other major csv | other lile csv | other ree csv | other hfse csv | other hpe csv | other tm csv | other misc csv | |
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54-Sn-264 | 53.88707 | -166.93202 | Snyder, G. L. | 1954-01-01 | Makushin | Granodiorite and related rocks from 4 mi E of Cape Starichkof. Elevation 1,000 feet on the west-facing hill slope 2 3/4 miles southwest of Tarasof Point. | Quartz gabbro from elevation 1,000 feet on the west-facing hill slope 2 3/4 miles southwest of Tarasof Point. The texture is hypidiomorphic-granular. Felsic minerals compose 75-80 percent of the rock: 4-6 percent quartz, <0.1 percent orthoclase, and 70-75 percent plagioclase slightly altered to sericite (<0.1 percent). The plagioclase composition, by extinction angle, is An54 [mean of 36 crystals, standard deviation is 7 percent An, average amount of zoning per individual plagioclase crystal is 9 percent An per crystal]. Mafic minerals compose 20-25 percent: 0.5-1.5 percent clinopyroxene (remnants in hornblende and euhedra in feldspar), 8-10 percent hornblende (an indeterminate amount derived from clinopyroxene), 6-8 percent biotite slightly altered to penninite (<0.1 percent) and cliozoisite (<0.1 percent), 2-5 percent magnetite, <0.1 percent hematite, 0.5-1.5 percent apatite, 0.5-1 percent tourmaline, and 0.1-1 percent penninite (interstitial). | 54-Sn-264 | Countryrock | Enclave/Inclusion | Whole-rock | 54.9 | 0.94 | 18.6 | 7.1 | 0.16 | 4.5 | 7.8 | 3.6 | 1.1 | 0.22 | Total not given in table. 99.78 | 315 | RAPIDA | 2.6 | 4.8 | H2OM=0.08; H2OP=0.77; CO2=0.05; Cl=0.1; F=0.01 | RAPIDA |
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