Unspiked K–Ar dating of Pleistocene tholeiitic basalts from the deep core SOH-4, Kilauea, Hawaii
Tholeiitic subaerial lava flows from Kilauea (SOH-4 deep core) were successfully dated by unspiked K–Ar with 40Ar * contents as low as ≈0.1%. Ages between 436 and 42 ka were found on lavas between the depths of 1650 and 468 m. All subaerial ages are consistent with their stratigraphic position and a...
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Veröffentlicht in: | Chemical geology 1997-06, Vol.140 (1), p.81-88 |
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creator | Guillou, Hervé Turpin, Laurent Garnier, Florence Charbit, Sylvie Thomas, Don M |
description | Tholeiitic subaerial lava flows from Kilauea (SOH-4 deep core) were successfully dated by unspiked K–Ar with
40Ar
* contents as low as ≈0.1%. Ages between 436 and 42 ka were found on lavas between the depths of 1650 and 468 m. All subaerial ages are consistent with their stratigraphic position and allow us to derive a lava accumulation rate of 3.07±0.44 mm/a, which is within the range of rates determined in high
40Ar
* OIBs. Age determinations on dike samples yield ages that are younger than those of the enclosing lavas. The validity of the ages was cross-checked with U-series ages of coral terraces on the northwest flank of Hawaii as determined by
Ludwig et al. (1991). Dating problems seem to be restricted to a submarine pillow lava sample from level 1808 m, which gives an apparent age of ≈1 Ma, which is an overestimate with respect both to rate of construction of Kilauea and the Hawaiian plume history. |
doi_str_mv | 10.1016/S0009-2541(97)00044-2 |
format | Article |
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40Ar
* contents as low as ≈0.1%. Ages between 436 and 42 ka were found on lavas between the depths of 1650 and 468 m. All subaerial ages are consistent with their stratigraphic position and allow us to derive a lava accumulation rate of 3.07±0.44 mm/a, which is within the range of rates determined in high
40Ar
* OIBs. Age determinations on dike samples yield ages that are younger than those of the enclosing lavas. The validity of the ages was cross-checked with U-series ages of coral terraces on the northwest flank of Hawaii as determined by
Ludwig et al. (1991). Dating problems seem to be restricted to a submarine pillow lava sample from level 1808 m, which gives an apparent age of ≈1 Ma, which is an overestimate with respect both to rate of construction of Kilauea and the Hawaiian plume history.</description><identifier>ISSN: 0009-2541</identifier><identifier>EISSN: 1872-6836</identifier><identifier>DOI: 10.1016/S0009-2541(97)00044-2</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>accumulation rate ; Continental interfaces, environment ; Kilauea ; Ocean, Atmosphere ; Sciences of the Universe ; tholeiites ; unspiked K–Ar dating</subject><ispartof>Chemical geology, 1997-06, Vol.140 (1), p.81-88</ispartof><rights>1997 Elsevier Science B.V.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a430t-8c9f5327bb68fca548589671217bad728222095033b2b43b1a7397ad7384df673</citedby><cites>FETCH-LOGICAL-a430t-8c9f5327bb68fca548589671217bad728222095033b2b43b1a7397ad7384df673</cites><orcidid>0000-0002-4811-7668</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0009254197000442$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,776,780,881,3537,27901,27902,65306</link.rule.ids><backlink>$$Uhttps://hal.science/hal-03357026$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Guillou, Hervé</creatorcontrib><creatorcontrib>Turpin, Laurent</creatorcontrib><creatorcontrib>Garnier, Florence</creatorcontrib><creatorcontrib>Charbit, Sylvie</creatorcontrib><creatorcontrib>Thomas, Don M</creatorcontrib><title>Unspiked K–Ar dating of Pleistocene tholeiitic basalts from the deep core SOH-4, Kilauea, Hawaii</title><title>Chemical geology</title><description>Tholeiitic subaerial lava flows from Kilauea (SOH-4 deep core) were successfully dated by unspiked K–Ar with
40Ar
* contents as low as ≈0.1%. Ages between 436 and 42 ka were found on lavas between the depths of 1650 and 468 m. All subaerial ages are consistent with their stratigraphic position and allow us to derive a lava accumulation rate of 3.07±0.44 mm/a, which is within the range of rates determined in high
40Ar
* OIBs. Age determinations on dike samples yield ages that are younger than those of the enclosing lavas. The validity of the ages was cross-checked with U-series ages of coral terraces on the northwest flank of Hawaii as determined by
Ludwig et al. (1991). Dating problems seem to be restricted to a submarine pillow lava sample from level 1808 m, which gives an apparent age of ≈1 Ma, which is an overestimate with respect both to rate of construction of Kilauea and the Hawaiian plume history.</description><subject>accumulation rate</subject><subject>Continental interfaces, environment</subject><subject>Kilauea</subject><subject>Ocean, Atmosphere</subject><subject>Sciences of the Universe</subject><subject>tholeiites</subject><subject>unspiked K–Ar dating</subject><issn>0009-2541</issn><issn>1872-6836</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><recordid>eNqFkM1KAzEUhYMoWKuPIGRpoaP5mUwyKylFHWmhQu06JJmMjU5nSjJW3PkOvqFPYtpKt64u597zHbgHgEuMrjHC2c0cIZQnhKX4KueDKNI0IUeghwUnSSZodgx6B8spOAvhNUpMGesBvWjC2r3ZEk5-vr5HHpaqc80LbCv4VFsXutbYxsJu2UblOmegVkHVXYCVb1dxb2Fp7Rqa1ls4nxVJOoQTV6t3q4awUB_KuXNwUqk62Iu_2QeL-7vncZFMZw-P49E0USlFXSJMXjFKuNaZqIxiqWAizzgmmGtVciIIIShniFJNdEo1VpzmPF6oSMsq47QPBvvcparl2ruV8p-yVU4Wo6nc7iLKOCLZBkcv23uNb0PwtjoAGMltqXJXqtw2JnMud6VKErnbPWfjIxtnvQzG2cbY0nlrOlm27p-EX_IdfJw</recordid><startdate>199706</startdate><enddate>199706</enddate><creator>Guillou, Hervé</creator><creator>Turpin, Laurent</creator><creator>Garnier, Florence</creator><creator>Charbit, Sylvie</creator><creator>Thomas, Don M</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0002-4811-7668</orcidid></search><sort><creationdate>199706</creationdate><title>Unspiked K–Ar dating of Pleistocene tholeiitic basalts from the deep core SOH-4, Kilauea, Hawaii</title><author>Guillou, Hervé ; Turpin, Laurent ; Garnier, Florence ; Charbit, Sylvie ; Thomas, Don M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a430t-8c9f5327bb68fca548589671217bad728222095033b2b43b1a7397ad7384df673</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1997</creationdate><topic>accumulation rate</topic><topic>Continental interfaces, environment</topic><topic>Kilauea</topic><topic>Ocean, Atmosphere</topic><topic>Sciences of the Universe</topic><topic>tholeiites</topic><topic>unspiked K–Ar dating</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Guillou, Hervé</creatorcontrib><creatorcontrib>Turpin, Laurent</creatorcontrib><creatorcontrib>Garnier, Florence</creatorcontrib><creatorcontrib>Charbit, Sylvie</creatorcontrib><creatorcontrib>Thomas, Don M</creatorcontrib><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Chemical geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Guillou, Hervé</au><au>Turpin, Laurent</au><au>Garnier, Florence</au><au>Charbit, Sylvie</au><au>Thomas, Don M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Unspiked K–Ar dating of Pleistocene tholeiitic basalts from the deep core SOH-4, Kilauea, Hawaii</atitle><jtitle>Chemical geology</jtitle><date>1997-06</date><risdate>1997</risdate><volume>140</volume><issue>1</issue><spage>81</spage><epage>88</epage><pages>81-88</pages><issn>0009-2541</issn><eissn>1872-6836</eissn><abstract>Tholeiitic subaerial lava flows from Kilauea (SOH-4 deep core) were successfully dated by unspiked K–Ar with
40Ar
* contents as low as ≈0.1%. Ages between 436 and 42 ka were found on lavas between the depths of 1650 and 468 m. All subaerial ages are consistent with their stratigraphic position and allow us to derive a lava accumulation rate of 3.07±0.44 mm/a, which is within the range of rates determined in high
40Ar
* OIBs. Age determinations on dike samples yield ages that are younger than those of the enclosing lavas. The validity of the ages was cross-checked with U-series ages of coral terraces on the northwest flank of Hawaii as determined by
Ludwig et al. (1991). Dating problems seem to be restricted to a submarine pillow lava sample from level 1808 m, which gives an apparent age of ≈1 Ma, which is an overestimate with respect both to rate of construction of Kilauea and the Hawaiian plume history.</abstract><pub>Elsevier B.V</pub><doi>10.1016/S0009-2541(97)00044-2</doi><tpages>8</tpages><orcidid>https://orcid.org/0000-0002-4811-7668</orcidid></addata></record> |
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source | Elsevier ScienceDirect Journals |
subjects | accumulation rate Continental interfaces, environment Kilauea Ocean, Atmosphere Sciences of the Universe tholeiites unspiked K–Ar dating |
title | Unspiked K–Ar dating of Pleistocene tholeiitic basalts from the deep core SOH-4, Kilauea, Hawaii |
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