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

Lawrence, James R; Natland, James H (1982): (Table 1) Oxygen isotope temperatures from hydrothermally altered breccias at DSDP Hole 60-453 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.820226, Supplement to: Lawrence, JR; Natland, JH (1982): Temperatures of hydrothermal alteration in Deep Sea Drilling Project Hole 453, western Mariana Trough. In: Hussong, DM; Uyeda, S; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 60, 755-758, https://doi.org/10.2973/dsdp.proc.60.143.1982

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

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Gabbro-metabasalt polymict breccias cored in Deep Sea Drilling Project Hole 453 are cemented in part by hydrothermal alteration to lower greenschist facies (chlorite-epidote-actinolite) mineral assemblages. Temperature estimates for this alteration, based on oxygen isotope determinations of secondary minerals, are nearly 100°C at the top of the breccias and over 200°C in a zone of intense alteration near the base.
Project(s):
Coverage:
Latitude: 17.907000 * Longitude: 143.682500
Date/Time Start: 1978-03-28T00:00:00 * Date/Time End: 1978-03-28T00:00:00
Minimum Elevation: -4693.0 m * Maximum Elevation: -4693.0 m
Event(s):
60-453 * Latitude: 17.907000 * Longitude: 143.682500 * Date/Time: 1978-03-28T00:00:00 * Elevation: -4693.0 m * Penetration: 605 m * Recovery: 235.1 m * Location: North Pacific/SEDIMENT POND * Campaign: Leg60 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 63 cores; 595.5 m cored; 9.5 m drilled; 39.5 % recovery
Comment:
Analyses were made according to the method of Clayton and Mayeda (1963) but utilized O2 gas in a 6-in. Nuclide mass spectrometer housed at Lamont-Doherty Geological Observatory instead of converting it to CO2. The mass spectrometer reference gas, tank O2, was calibrated using NBS-28, which was assumed to have a 1 8O = +10.0 per mil (SMOW), as given in Friedman and Gleason (1973).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample code/labelSample labelLawrence, James RDSDP/ODP/IODP sample designation
IdentificationIDLawrence, James R
Mineral nameMineralLawrence, James R
δ18Oδ18OLawrence, James Rsee commentSMOW
δ18O, standard deviationδ18O std dev±Lawrence, James Rsee comment
Temperature, calculatedT cal°CLawrence, James R
Size:
16 data points

Data

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


Sample label

ID

Mineral

δ18O []

δ18O std dev [±]

T cal [°C]
60-453-49-1,3-5#1Quartz20.20.3107
60-453-55-1,45-46#2EPotassium feldspar18.295
60-453-57-2,83-89#13Potassium feldspar9.3206