Calcite U–Pb dating of altered ancient oceanic crust in the North Pamir, Central Asia
J. Rembe,
R. Zhou,
E. R. Sobel,
J. Kley,
J. Chen,
J.-X. Zhao,
Y. Feng,
D. L. Howard
Affiliations
J. Rembe
Institute of Geosciences, University of Potsdam, 14476 Potsdam, Germany
R. Zhou
School of Earth and Environmental Sciences, The University of Queensland, St Lucia, Brisbane, QLD 4072, Australia
E. R. Sobel
Institute of Geosciences, University of Potsdam, 14476 Potsdam, Germany
J. Kley
Department of Structural Geology and Geodynamics, Georg-August-Universität Göttingen, 37077 Göttingen, Germany
J. Chen
State Key Lab. of Earthquake Dynamics, Xinjiang Pamir Intracontinental Subduction National Field Observation and Research Station, Institute of Geology, China Earthquake Administration, X9GJ+RV Chaoyang, Beijing, China
J.-X. Zhao
School of Earth and Environmental Sciences, The University of Queensland, St Lucia, Brisbane, QLD 4072, Australia
Y. Feng
School of Earth and Environmental Sciences, The University of Queensland, St Lucia, Brisbane, QLD 4072, Australia
D. L. Howard
The Australian Synchrotron, 800 Blackburn Rd, Clayton, VIC 3168, Australia
The North Pamir, part of the western syntax of the India–Asia collision zone, preserves remnants of a poorly understood Paleozoic intra-oceanic subduction zone. To constrain the age of this ancient ocean floor, we analyzed calcite phases in vesicular basalt and basaltic volcanic breccia with U–Pb geochronology using laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). Dating of radial fibrous to equant spary calcite yielded three meaningful Visean–Serpukhovian ages. Rare-earth elements and yttrium (REE + Y) data reveal that the basaltic host rock of the calcite and oxidizing seawater are major sources of trace elements during calcite precipitation. U–Pb ages seem to be independent of REE + Y concentrations. Our results demonstrate the potential of calcite dating to constrain the age of ancient ocean floors. We challenge the hypothesis that a continuous early Paleozoic Kunlun Terrane extended from northern Tibet into the North Pamir.
