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Island arc tectonics of New Zealand manifested in helium isotope ratios

Journal Article · · Geochim. Cosmochim. Acta; (United States)
Thirty gas samples of various types - volcanic gas, geothermal gas, CH/sub 4/-rich natural gas, and petroleum gas - were collected in and around the North Island, New Zealand. /sup 3/He//sup 4/He and /sup 4/He//sup 20/Ne ratios were measured using a mass spectrometer. The observed /sup 3/He//sup 4/He and /sup 4/He//sup 20/Ne ratios of the samples varied from 0.08 x 10/sup -6/ to 8.75 x 10/sup -6/ and from 4.8 to 2100, respectively. Based on a /sup 3/He//sup 4/He-/sup 4/He//sup 20/Ne diagram, He in the samples can be explained by mixing of a subduction-type magmatic, a radiogenic, and an air component. The geographical distribution of /sup 3/He//sup 4/He ratios over the island indicates a clear contrast between forearc and volcanic arc regions: high in the former and low in the latter. A He boundary can be drawn from the Taupo Volcanic Zone to Egmont Volcano in terms of the /sup 3/He//sup 4/He profile. This boundary agrees well with that of high Q/low Q in the upper mantle as well as with the geographical distribution of terrestrial heat flow values. The high /sup 3/He//sup 4/He ratios in the volcanic arc region are attributed to subduction-type He associated with an uprising magma from the upper mantle and the lower ratios in the forearc region to radiogenic He derived from U and Th in basement and sedimentary rocks. This tendency is very similar to that found in northeast Japan and is understood to be a general signature of the He isotope ratio in an island arc system.
Research Organization:
Univ. of Tokyo (Japan)
OSTI ID:
7222728
Journal Information:
Geochim. Cosmochim. Acta; (United States), Journal Name: Geochim. Cosmochim. Acta; (United States) Vol. 51:7; ISSN GCACA
Country of Publication:
United States
Language:
English