Citation:

odp.proc.sr.135.161.1994

Name: Geochemistry of ODP Hole 135-839B lavas
Published: 1994
License: https://creativecommons.org/licenses/by/3.0/

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Abstract:

Four petrographic lava types occur, ranging from aphyric to moderately phyric clinopyroxene-olivine tholeiitic basalts (Unit 1); olivine-clinopyroxene picritic basalts, sparsely to strongly olivine-phyric (Unit 3-type); olivine-clinopyroxene basalts (clinopyroxene dominant) (Unit 4); and moderately to strongly phyric two-pyroxene-plagioclase basaltic andesites (Unit 9-type). The olivine phyric lavas contain forsteritic olivines (extending to Fo92), and very magnesian Cr-rich spinels similar to those occurring in boninitic lavas. The basaltic andesites are mineralogically and petrographically indistinguishable from the modern Tofua Arc basaltic andesites, one notable feature being the highly calcic cores in plagioclase phenocrysts (up to An95). The forsteritic olivines, the Cr-spinels, and the calcic plagioclases are unlikely to have been precipitated in the lava compositions in which they occur, and are thought to have been incorporated from highly primitive melts by way of mixing processes (as advocated by Allan, this volume). Notwithstanding the evidence for mixing, the major element chemistries of the Unit 1- and Unit 9-type lavas are shown to be consistent with the derivation of the Unit 9-type basaltic andesites by means of fractional crystallization, through magmas of similar chemistry to Unit 1. Some trace element discrepancies in the modeling, and the relative volcanic stratigraphy of Site 839, however, preclude a direct liquid line of descent between the actual recovered units.

Trace element data as well as TiO2 and Na2O data clearly illustrate the arc-like affinities of the magmas, with strong highfield-strength element depletion and large-ion-lithophile element enrichment. The abundance patterns are very close to those of the Tofua and Kermadec arc magmas, and also Valu Fa.

Pb-, Sr-, and Nd-isotopic compositions indicate closest affinities with a "Pacific" MORB source, apparently characteristic of the western, older part of the Lau Basin. A subduction-related isotopic contribution is, however, inferred. The sources of the Site 839 magmas are thus inferred to be similar to, but less depleted geochemically, than those of the modern Tofua Arc magmas. The Site 839 sequence is interpreted as an older remnant of a volcanic construct of the "proto-Tofua arc", originally developed adjacent to the Tonga Ridge. Opening of the eastern Lau Basin, because of southward migrating propagators, has split and isolated the sequence, leaving it stranded within the modern Lau Basin.

Project(s):

Ocean Drilling Program (ODP)

Coverage:

Latitude: -20.709000 * Longitude: -176.775000

Date/Time Start: 1991-01-17T16:00:00 * Date/Time End: 1991-01-24T00:40:00

Event(s):

135-839B * Latitude: -20.709000 * Longitude: -176.775000 * Date/Time Start: 1991-01-17T16:00:00 * Date/Time End: 1991-01-24T00:40:00 * Elevation: -2629.0 m * Penetration: 517.2 m * Recovery: 25.05 m * Location: South Pacific Ocean * Campaign: * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 42 cores; 356.6 m cored; 0 m drilled; 7 % recovery

License:

Creative Commons Attribution 3.0 Unported (CC-BY-3.0)

Size:

2 datasets

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Datasets listed in this publication series

Ewart, A; Hergt, JM; Hawkins, JW (1994): (Table 1) Major, trace element and isotopic composition of ODP Hole 135-839B lavas. https://doi.org/10.1594/PANGAEA.793075
Ewart, A; Hergt, JM; Hawkins, JW (1994): (Table 2) Geochemistry for numerical modelling of ODP Hole 135-839B lavas. https://doi.org/10.1594/PANGAEA.793076