40Ar-39Ar geochronological studies on rocks drilled at DSDP Holes 61-462 and 61-462A


Autoria(s): Ozima, Minoru; Saito, K; Takigami, Yutaka
Cobertura

MEDIAN LATITUDE: 7.239600 * MEDIAN LONGITUDE: 165.031100 * SOUTH-BOUND LATITUDE: 7.237500 * WEST-BOUND LONGITUDE: 165.030500 * NORTH-BOUND LATITUDE: 7.241700 * EAST-BOUND LONGITUDE: 165.031700 * DATE/TIME START: 1978-05-28T00:00:00 * DATE/TIME END: 1978-06-09T00:00:00

Data(s)

02/10/1981

Resumo

40Ar-39Ar step-heating dating was applied to a basalt from Hole 462 and to basalt and dolerite samples from Hole 462A. Only a basalt sample at Hole 462A yielded a reasonable isochron age, 110 ± 3 million years. The radiometric age is consistent with the fossil record (Cenomanian) in the sediments, into which the basalt sill intruded. However, the age is much less than that of the oceanic basement as deduced from the magnetic anomaly (M-26).

Formato

application/zip, 2 datasets

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.819947

doi:10.1594/PANGAEA.819947

Idioma(s)

en

Publicador

PANGAEA

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

Supplement to: Ozima, Minoru; Saito, K; Takigami, Yutaka (1981): 40Ar-39Ar geochronological studies on rocks drilled at Holes 462 and 462A, Deep Sea Drilling Project Leg 61. In: Larson, RL; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 61, 701-703, doi:10.2973/dsdp.proc.61.128.1981

Palavras-Chave #-; 37Ar/36Ar; 37Ar/36Ar e rel; 39Ar; 39Ar/36Ar; 39Ar/36Ar e rel; 40Ar/36Ar; 40Ar/36Ar e rel; 61-462; 61-462A; Age, dated; Age, dated standard deviation; Age dated; Age std dev; Apparent; # = about; Apparent; # = about; 1 sigma; Argon-37/Argon-36; Argon-37/Argon-36, error, relative; Argon-39; Argon-39/Argon-36; Argon-39/Argon-36, error, relative; Argon-40/Argon-36; Argon-40/Argon-36, error, relative; Comment; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Event; Fusion; Glomar Challenger; Isocrhon age; MSUM = SUMS/N-2. N = number of fractions (Brooks et al., 1972).; J; Label; Leg61; ODP sample designation; Plateau age; Only for the fusion fraction, which constitutes more than 80% of the 39Ar released; Rock; Rock type; Sample code/label; see reference(s); Temperature, technical; Total fusion age = 1/lambda ln [1 + J(40Ar/39Ar)total]* (40Ar/39Ar)total = Sum-fi (40Ar/39Ar)i*fi = 39Ar fraction released; T tech
Tipo

Dataset