(Table 1) K-Ar age of alkaline igneous rocks from the Jan Mayen fracture zone

Fuente: PANGAEA
Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: Kharin, Gennady S, Pustovoi, A A
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 1996
Schlagworte:
Online-Zugang:
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
_version_ 1867169981767090176
author Kharin, Gennady S
Pustovoi, A A
author_facet Kharin, Gennady S
Pustovoi, A A
collection Datos científicos de ciencias marinas y ambientales
contents Bottom morphology of the Jan Mayen transform fracture zone and rock chemistry data show that petrological and chemical specific features of igneous rocks can result from higher permeability of the transform fracture zone and deeper penetration of ocean water into the lithosphere in comparison with rift zones of the Kolbeinsey and Mohn's mid-ocean ridges. Age of alkaline magmatism of the Jan Mayen fracture zone is similar to that of rift zones due to palingenesis of metamorphosed and hydrated mantle and crustal rocks.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_762254
institution PANGAEA
language en
publishDate 1996
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) K-Ar age of alkaline igneous rocks from the Jan Mayen fracture zone
Kharin, Gennady S
Pustovoi, A A
38-343; 38-345; Age, dated; Archive of Ocean Data; ARCOD; Argon-40; Argon-40/Potassium-40; B77-154; Calculated; Dredge; DRG; DRILL; Drilling/drill rig; Elevation of event; Elevation of event 2; Event label; Glomar Challenger; Jan Mayen transform fracture zone; KhP-13; KhP-769; KhP-794; Latitude of event; Leg38; Longitude of event; Mass spectrometry (MS); North Atlantic/Norwegian Sea/BASIN; Potassium-40; Potassium oxide; Rock type; Sample code/label; Wet chemistry
Bottom morphology of the Jan Mayen transform fracture zone and rock chemistry data show that petrological and chemical specific features of igneous rocks can result from higher permeability of the transform fracture zone and deeper penetration of ocean water into the lithosphere in comparison with rift zones of the Kolbeinsey and Mohn's mid-ocean ridges. Age of alkaline magmatism of the Jan Mayen fracture zone is similar to that of rift zones due to palingenesis of metamorphosed and hydrated mantle and crustal rocks.
title (Table 1) K-Ar age of alkaline igneous rocks from the Jan Mayen fracture zone
topic 38-343; 38-345; Age, dated; Archive of Ocean Data; ARCOD; Argon-40; Argon-40/Potassium-40; B77-154; Calculated; Dredge; DRG; DRILL; Drilling/drill rig; Elevation of event; Elevation of event 2; Event label; Glomar Challenger; Jan Mayen transform fracture zone; KhP-13; KhP-769; KhP-794; Latitude of event; Leg38; Longitude of event; Mass spectrometry (MS); North Atlantic/Norwegian Sea/BASIN; Potassium-40; Potassium oxide; Rock type; Sample code/label; Wet chemistry
url https://doi.org/10.1594/PANGAEA.762254