![](/images/icons/spacer.gif) |
Detailed Reference Information |
Sharp, W.D. and Renne, P.R. (2005). The 40Ar/39Ar dating of core recovered by the Hawaii Scientific Drilling Project (phase 2), Hilo, Hawaii. Geochemistry Geophysics Geosystems 6: doi: 10.1029/2004GC000846. issn: 1525-2027. |
|
The Hawaii Scientific Drilling Project, phase 2 (HSDP-2), recovered core from a ~3.1-km-thick section through the eastern flanks of Mauna Loa and Mauna Kea volcanoes. We report results of 40Ar/39Ar incremental heating by broad-beam infrared laser of 16 basaltic groundmass samples and 1 plagioclase separate, mostly from K-poor tholeiites. The tholeiites generally have mean radiogenic 40Ar enrichments of 1--3%, and some contain excess 40Ar; however, isochron ages of glass-poor samples preserve stratigraphic order in all cases. A 246-m-thick sequence of Mauna Loa tholeiitic lavas yields an isochron age of 122 ¿ 86 kyr (all errors 2σ) at its base. Beneath the Mauna Loa overlap sequence lie Mauna Kea's postshield and shield sequences. A postshield alkalic lava yields an age of 236 ¿ 16 kyr, in agreement with an age of 240 ¿ 14 kyr for a geochemically correlative flow in the nearby HSDP-1 core hole, where more complete dating of the postshield sequence shows it to have accumulated at 0.9 ¿ 0.4 m/kyr, from about 330 to <200 ka. Mauna Kea's shield consists of subaerial tholeiitic flows to a depth of 1079 m below sea level, then shallow submarine flows, hyaloclastites, pillow lavas, and minor intrusions to core bottom at 3098 m. Most subaerial tholeiitic flows fail to form isochrons; however, a sample at 984 m yields an age of 370 ¿ 180 kyr, consistent with ages from similar levels in HSDP-1. Submarine tholeiites including shallow marine vitrophyres, clasts from hyaloclastites, and pillow lavas were analyzed; however, only pillow lava cores from 2243, 2614, and 2789 m yield reliable ages of 482 ¿ 67, 560 ¿ 150, and 683 ¿ 82 kyr, respectively. A linear fit to ages for shield samples defines a mean accumulation rate of 8.6 ¿ 3.1 m/kyr and extrapolates to ~635 kyr at core bottom. Alternatively, a model relating Mauna Kea's growth to transport across the Hawaiian hot spot that predicts downward accelerating accumulation rates that reach ~20 m/kyr at core bottom (DePaolo and Stolper, 1996) is also consistent with all reliable ages except the deepest. |
|
![](/images/icons/spacer.gif) |
![](/images/icons/spacer.gif) |
BACKGROUND DATA FILES |
|
![](../images/icons/sq.gif) |
Abstract![](/images/icons/spacer.gif) |
|
![](../images/buttons/download.very.flat.gif) |
|
|
|
Keywords
Geochronology, Quaternary geochronology, Geochronology, Radioisotope geochronology, Marine Geology and Geophysics, Oceanic hotspots and intraplate volcanism, Mineralogy and Petrology, Intra-plate processes (1033, 8415), Volcanology, Intra-plate processes (1033, 3615), Ar-Ar dating, ocean island basalt, Quaternary dating, volcanology |
|
Journal
Geochemistry Geophysics Geosystems |
|
Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
|
|
![](/images/icons/spacer.gif) |