Vein mineral ages of oceanic crust from the Atlantic Ocean

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Autori principali: Richardson, Stephen H, Hart, Stanley R, Staudigel, Hubert
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1980
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author Richardson, Stephen H
Hart, Stanley R
Staudigel, Hubert
author_facet Richardson, Stephen H
Hart, Stanley R
Staudigel, Hubert
collection Datos científicos de ciencias marinas y ambientales
contents Vein smectites with large Rb/Sr enrichments from extensively altered basaltic oceanic crust in Deep Sea Drilling Project hole 417A in the western Atlantic define a highly constrained Rb/Sr isochron age of 108 +/- 3 m.y. This age is identical to a less well constrained age of 108 +/- 17 m.y. for vein smectites with lower Rb/Sr enrichments from adjacent hole 418A and to the 108 m.y. age of crust formation derived by paleontological and magnetic anomaly correlation. Reasonable agreement exists between the 87Sr/86Sr ratio of vein calcites from both sites and the seawater 87Sr/86Sr ratio at the time. Pervasive low-temperature alteration in the contrasting environments of sites 417 and 418 appears to be coeval and essentially coincident with basement formation. Alteration may be used to advantage in determining ages of old oceanic crust.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_708671
institution PANGAEA
language en
publishDate 1980
publisher PANGAEA
record_format pangaea
spellingShingle Vein mineral ages of oceanic crust from the Atlantic Ocean
Richardson, Stephen H
Hart, Stanley R
Staudigel, Hubert
51-417A; 52-418A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg51; Leg52; North Atlantic/CONT RISE
Vein smectites with large Rb/Sr enrichments from extensively altered basaltic oceanic crust in Deep Sea Drilling Project hole 417A in the western Atlantic define a highly constrained Rb/Sr isochron age of 108 +/- 3 m.y. This age is identical to a less well constrained age of 108 +/- 17 m.y. for vein smectites with lower Rb/Sr enrichments from adjacent hole 418A and to the 108 m.y. age of crust formation derived by paleontological and magnetic anomaly correlation. Reasonable agreement exists between the 87Sr/86Sr ratio of vein calcites from both sites and the seawater 87Sr/86Sr ratio at the time. Pervasive low-temperature alteration in the contrasting environments of sites 417 and 418 appears to be coeval and essentially coincident with basement formation. Alteration may be used to advantage in determining ages of old oceanic crust.
title Vein mineral ages of oceanic crust from the Atlantic Ocean
topic 51-417A; 52-418A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg51; Leg52; North Atlantic/CONT RISE
url https://doi.org/10.1594/PANGAEA.708671