Christie, David M.; Pedersen, Rolf B.; Miller, D. Jay; Balzer, Vaughn G.; Einaudi, Florence; Gee, M. A. Mary; Hauff, Folkmar; Kempton, Pamela D.; Liang, Wen-Tzong; Lysnes, Kristine; Meyzen, Christine M.; Pyle, Douglas G.; Russo, Christopher J.; Sato, Hiroshi; Thorseth, Ingunn H. (2001): Site 1158. Texas A&M University, Ocean Drilling Program, College Station, TX, United States, In: Christie, David M., Pedersen, Rolf B., Miller, D. Jay, Balzer, Vaughn G., Einaudi, Florence, Gee, M. A. Mary, Hauff, Folkmar, Kempton, Pamela D., Liang, Wen-Tzong, Lysnes, Kristine, Meyzen, Christine M., Pyle, Douglas G., Russo, Christopher J., Sato, Hiroshi, Thorseth, Ingunn H., Bridges, Brenda (editor), Proceedings of the Ocean Drilling Program, initial reports, mantle reservoirs and migration associated with Australian Antarctic rifting; covering Leg 187 of the cruises of the drilling vessel JOIDES Resolution; Fremantle, Australia, to Fremantle, Australia; sites 1152-1164, 16 November 1999-10 January 2000, 187, georefid:2003-045871

Abstract:
Site 1158 was located in Zone A, and was one of six sites along a generally north-south line that were intended to locate possible occurrences of Indian-type mantle beneath western Zone A Hole 1158A produced 0.8 m (5.9% recovery) of aphyric to sparsely olivine plagioclase phyric basalt with a few glassy rinds. It was abandoned because of poor drilling conditions Hole 1158B yielded 1.6 m (10.7% recovery) of aphyric to sparsely olivine plagioclase phyric basalt. The basalt is slightly to moderately altered. It too was abandoned because of poor drilling conditions. Hole 1158C yielded 1.61 m (17.1%) of massive diabase (composed of plagioclase, clinopyroxene, and magnetite/ilmenite with a medium-grained subophitic texture) beneath overlying aphyric basalt rubble. Two lithologic units were identified. Unit 1 was similar to A and B and Unit 2 was a diabase. Low-temperature alteration products were present throughout this core. Ba and Zr systematics indicate that Site 1158 lavas were derived from Pacific-type mantle <2 mu after the Indian-type lavas of Site 1157 were erupted on the same flow line. Igneous petrology, alteration, microbiology, structural geology, site geophysics, sediments, and geochemistry studies were carried out. Data tables and figures are found at the end of the chapter.(LEL)
Coverage:
West: 128.4942 East: 128.4942 North: -43.5642 South: -43.5654
Relations:
Expedition: 187
Site: 187-1158
Supplemental Information:
Available only on CD-ROM and on the Web in PDF format
Data access:
Provider: SEDIS Publication Catalogue
Data set link: http://sedis.iodp.org/pub-catalogue/index.php?id=10.2973/odp.proc.ir.189.109.2001 (c.f. for more detailed metadata)
Data download: application/pdf
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