Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Kono, Masaru; Clague, David A; Larson, Edwin E (1980): (Table 2) Reflection microscopy of Fe-Ti oxides at DSDP Hole 55-432A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.823365, In supplement to: Kono, M et al. (1980): Fe-Ti oxide mineralogy of DSDP Leg 55 basalts. In: Jackson, ED; Koisumi, I; et al., (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 55, 639-652, https://doi.org/10.2973/dsdp.proc.55.126.1980

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Project(s):
Coverage:
Latitude: 41.333800 * Longitude: 170.379000
Date/Time Start: 1977-08-06T00:00:00 * Date/Time End: 1977-08-06T00:00:00
Minimum Elevation: -1310.0 m * Maximum Elevation: -1310.0 m
Event(s):
55-432A * Latitude: 41.333800 * Longitude: 170.379000 * Date/Time: 1977-08-06T00:00:00 * Elevation: -1310.0 m * Penetration: 74 m * Recovery: 16.1 m * Location: North Pacific/TERRACE * Campaign: Leg55 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 5 cores; 38 m cored; 0 m drilled; 42.4 % recovery
Comment:
+++ = abundant, ++ = common, + = present, - = absent.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample code/labelSample labelKono, MasaruDSDP/ODP/IODP sample designation
UnitUnitKono, MasaruFlow unit number and type of rock: A, alkalic basalts, T, tholeiites
Curie temperatureCurie temp°CKono, Masaru
TypeTypeKono, MasaruOptical microscopyType of thermomagnetic curve: NO, no oxidation, HT, high-temperature oxidation, LT, low-temperature oxidation
StageStageKono, MasaruOptical microscopyOxidation stage = degree of high-temperature oxidation of titanomagnetite: N, L, M, H = no, low, moderate, high oxidation
IlmeniteIlmKono, MasaruOptical microscopyPresence of ilmenite lamellae in (III) planes of (titano-) magnetite host crystal
PseudobrookitePsbKono, MasaruOptical microscopyPresence of pseudobrookite as oxidation product of Ti-rich phase
TitanomagnetiteTimagKono, MasaruOptical microscopyPresence of low-temperature oxidation product
CommentCommentKono, Masaru
Size:
97 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Sample label

Unit

Curie temp [°C]

Type

Stage

Ilm

Psb

Timag

Comment
55-432A-2-1,74-761 (A)373LTL-M+-+Early stage of maghemitization indicated by bluishgray tint and shrinkage cracks.
55-432A-2-1,107-1091 (A)364LTL-M+-+Low-grade maghemitization.
55-432A-2-2,23-252 (A)575HTH+++++-Silicate replacement abundant. Ilmenite lamellae replaced by pseudobrookite and hematite.
55-432A-2-2,72-742 (A)572HTM++++-Reddening of silicate common.
55-432A-2-3,12-142 (A)457LTL-M++-+Titanomagnetite shows blue-gray color. Shrinkage cracks present.
55-432A-2-3,21-232 (A)L-M++-++Moderate maghemitization.
55-432A-3-2,67-693 (A)187NON---Homogeneous equant titanomagnetite crystals of 20 µm or less. Brown color.
55-432A-4-1,64-663 (A)550HTM-H++++-Abundant replacement of silicates.
55-432A-4-1,120-1223 (A)391LTL-M++-++Wide ilmenite lamellae. Some big grains 20-100 µ_m.
55-432A-4-2,80-823 (A)577HTM+++-traceMaghemitization shown by bluish-gray color and shrinkage cracks.
55-432A-5-2,69-713 (A)299LTL-M+-+Pyrite is present, filling cracks in silicates and oxides.