Kurnosov, Victor B; Zolotarev, Boris P; Artamonov, Andrey V; Garanina, Svetlana A; Petrova, V; Eroshchev-Shak, Vadim A; Sokolova, Alla L (2003): (Table T4) Petrographic description of basalts and secondary minerals of altered volcanic rocks from ODP Hole 183-1137A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.785753, In supplement to: Kurnosov, VB et al. (2003): Data report: Alteration of basalts from the Kerguelen Plateau. In: Frey, FA; Coffin, MF; Wallace, PJ; Quilty, PG (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 183, 1-40, https://doi.org/10.2973/odp.proc.sr.183.013.2003
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -56.833050 * Longitude: 68.093450
Date/Time Start: 1998-12-31T21:00:00 * Date/Time End: 1999-01-06T16:40:00
Minimum Elevation: -1004.5 m * Maximum Elevation: -1004.5 m
Event(s):
183-1137A * Latitude: -56.833050 * Longitude: 68.093450 * Date/Time Start: 1998-12-31T21:00:00 * Date/Time End: 1999-01-06T16:40:00 * Elevation: -1004.5 m * Penetration: 371.2 m * Recovery: 219.38 m * Location: Indian Ocean * Campaign: Leg183 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 46 cores; 371.2 m cored; 0 m drilled; 59.1 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Kurnosov, Victor B | DSDP/ODP/IODP sample designation | ||
2 | Description | Description | Kurnosov, Victor B | Thin section analysis/measurements | ||
3 | Comment 2 (continued) | Comm 2 | Kurnosov, Victor B | Thin section analysis/measurements | ||
4 | Comment 3 (continued) | Comm 3 | Kurnosov, Victor B | Thin section analysis/measurements | ||
5 | Alteration | Alteration | Kurnosov, Victor B | Thin section analysis/measurements | smec = smectite, chl = chlorite, zeol = zeolite, PhX = phenocryst | |
6 | Alteration | Alteration | Kurnosov, Victor B | Thin section analysis/measurements | ..continued; smec = smectite, chl = chlorite, zeol = zeolite, PhX = phenocryst | |
7 | Minerals | Minerals | Kurnosov, Victor B | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
70 data points
Data
1 Sample label (DSDP/ODP/IODP sample designation) | 2 Description (Thin section analysis/measure...) | 3 Comm 2 (Thin section analysis/measure...) | 4 Comm 3 (Thin section analysis/measure...) | 5 Alteration (smec = smectite, chl = chlori...) | 6 Alteration (..continued; smec = smectite,...) | 7 Minerals (X-ray diffraction (XRD)) |
---|---|---|---|---|---|---|
183-1137A-25R-4,100-115 | Aphyric basalt, vesicular (20%-25%; 0.1-0.5 mm), incompletely crystallized. Groundmass with microdoleritic texture. | Phenocrysts of long lathe of plagioclase (andesine; 0.1-0.3 mm). Dark brown volcanic glass with opaque dust and clinopyroxene. | Moderate (30%-35%); vesicles completely or partly infilled by clay minerals, zeols, and carbonate. Oxidation of basalt is ~30%. | |||
183-1137A-27R-1,100-105 | Sparsely plagioclase microphyric basalt, vesicular (5%-10%; up to 2-4 mm), incompletely crystallized. | Groundmass of vitrophyric-microlitic texture. Phenocrysts of crystals of plagioclase (<1%; 0.5-0.6 mm). | ~25%-30%; clinopyroxene completely replaced by chl; plagiocl is partly replaced with chl; vesicles infilled zonally ... | ... (from walls to center of vesicles) with smec, zeol, and trace of chl, carbonate is located in center. Oxidation of basalt is low (~5%). | Smectite | |
183-1137A-29R-1,38-43 | Sparsely olivine-plagioclase microphyric basalt, weakly vesicular (1%; 0.1-0.3 mm), incompletely crystallized. | Groundmass intergranular partly microdoleritic texture. Microphenocrysts of single tabular crystals of plagiocl (andesine; to 0.2-0.4 mm) and olivine. | Groundmass of plagioclase lathe (50%), isometric clinopyroxene crystals (30%-35%), opaque minerals, and interstitial glass (5%-10%). | ~20%; olivine and interstitial glass completely replaced by smec and chl; vesicles infilled with smec and chl. Oxidation of basalt is low (~5%). | Smectite | |
183-1137A-29R-3,5-9 | Olivine-clinopyroxene-plagioclase phyric basalt, vesicular (10%-15%; 1-2 to 5 mm), incompletely crystallized. | Groundmass with vitrophyric-microlitic texture. Phenocrysts (5-10%) of olivine (0.2-0.7 mm), clinopyroxene (0.2-1 mm) and plagiocl (up to 1.3-1.5 mm). | Groundmass of plagioclase lathe (50%), clinopyroxene, and dark brown interstitial glass. | ~15%-20%; olivine and interstitial glass completely replaced by smec and chl; | vesicles infilled with smec and chl, with admixture of zeols and carbonate. Oxidation of basalt is low (~5%). | |
183-1137A-32R-3,71-76 | Clinopyroxene-plagioclase glomerophyric basalt, massive. | Phenocrysts of clinopyroxene (0.2-0.5 mm) and plagioclase (labradorite and andesine) (to 0.3-1.2 mm). | Groundmass of plagioclase lathe (45%-50%), clinopyroxene (30%-35%), opaque minerals (5%), and interstitial glass (10%). | 10%-15%; olivine replaced by smec, chl, and oxidized Fe, interstitial glass replaced by smec and chl. Oxidation of basalt is low (~2%). | Smectite and defective chlorite in trace amounts | |
183-1137A-32R-7,46-50 | The sample is similar to Sample 183-1137A-32R-3, 71-76 cm. | 10%-15%; olivine completely replaced by smec, chl, and oxidized Fe, interstitial glass replaced by smec and chl. Oxidation of basalt is low (~2%). | Smectite | |||
183-1137A-34R-3,18-23 | Contact of tuff and basalt: 1. Sparsely plagioclase microphyric basalt, weakly vesicular (single vesicles), incompletely crystallized. | Groundmass demonstrates microlitic texture. Microphenocrysts of plagioclase (<5%; to 0.1-0.55 mm). | Groundmass represented by glass and long lathe of plagioclase. | ~30%; microphenocrysts replaced completely by opaque minerals and traces of chl; interstitial glass replaced by chl and smec and opaque minerals. | Groundmass plagioclase replaced by albite; single vesicles infilled with opaque minerals and chl. Oxidation of basalt is moderate (~10%). | Smectite and hydromica, chlorite, and swelling chlorite in trace amounts |
183-1137A-34R-3,18-23 | Contact of tuff and basalt: 2. Crystal-lithoclastic tuff, vesicular. | Moderate (~30%). Oxidation of basalt is moderate (~10%). | Smectite and hydromica and quartz in trace amounts | |||
183-1137A-37R-5,73-79 | Sparsely plagioclase microphyric basalt, highly vesicular (~50%; 1-5 mm), incompletely crystallized, with microlitic texture in groundmass. | Microphenocrysts of plagioclase (<5%) represented by tabular crystals (0.1-0.3 mm). | Groundmass represented by interstitial glass and long plagioclase lathe. | ~60%; vesicles infilled (wall to center) with br-yellow chl, br-green chl with zeols (natrolite, tomsonite), green clay minerals with traces of zeols; | microPhX of plagiocl partly replaced by albite and chl; interst. glass replaced by opaques and chl. Oxidation of basalt strong (total ~40% of rock). | |
183-1137A-39R-2,114-119 | Aphyric basalt, incompletely crystallized, brecciated rock, with microlitic, partly hyaline, texture of groundmass. | ~35%; secondary minerals represented by chl, smec, and zeols. Oxidation of basalt is low (total ~3-5% of rock). | ||||
183-1137A-39R-3,6-14 | Sparsely plagioclase microphyric basalt, weakly vesicular, incompletely crystallized, with microlitic texture. | Microphenocrysts of plagioclase (<5%) represented by tabular crystals (0.2-1.2 mm). | Groundmass of plagioclase lathe, microlathe of clinopyroxene, opaque minerals, and interstitial glass. | Moderate (~30%); interstitial glass replaced by chl and smec; single vesicles infilled (from wall to center) with chl and smec. | Oxidation of basalt is low (total ~2% of rock). | Smectite |
183-1137A-43R-2,84-92 | Dacitic tuff. Matrix contains baked ashes. | Very high (80%); secondary minerals represented by chl and carbonate. Oxidation of basalt is moderate (total ~10%-15% of rock). | Smectite and quartz in trace amounts with 10% of mica layers | |||
183-1137A-45R-1,121-126 | Plagioclase phyric basalt, vesicular (10%-15%), incompletely crystallized, with microlitic, partly intersertal, texture. | Microphenocrysts of plagioclase (10%) are represented by tabular crystals. | Groundmass of plagioclase, clinopyroxene, and interstitial glass. | ~40%; olivine replaced by chl, plagiocl replaced by K-feldspar (adularia?), smec, chl and carbonate; interst. glass repl. by chl, smec, oxidized Fe; | single vesicles infilled with chl, smec, zeols, and carbonate. Oxidation of basalt is moderate (total ~10%-15% of rock). | Smectite and swelling chlorite and hydromica in trace amounts |