TY - JOUR
T1 - Data on recovery rates and external morphologies of zircon grains from mechanical and electrical pulverization of rock samples
AU - Takehara, Mami
AU - Horie, Kenji
AU - Hokada, Tomokazu
AU - Kiyokawa, Shoichi
N1 - Funding Information:
The authors appreciate the thoughtful comments and suggestions from Dr. M. Ostankovitch and the anonymous reviewers. This work was partially funded by the Japan Society for the Promotion of Science–Fund for the Promotion of Joint International Research ( JSPS KAKENHI ; grant numbers 25287132 and 17H02976 ) and the National Institute of Polar Research (NIPR; research projects KP–7 and KP–30 306). The production of this paper was supported by a NIPR publication subsidy.
Publisher Copyright:
© 2018 The Authors
PY - 2018/8
Y1 - 2018/8
N2 - In this data article, we provide information on the recovery rate and scanning electron microscope (SEM) images of the external morphology of zircon grains separated from two rock samples (AS3 and TEMORA 2) using both mechanical and electrical pulverization systems. The data in this article are related to the research article entitled “New insight into disturbance of U-Pb and trace-element systems in hydrothermally altered zircon via SHRIMP analyses of zircon from the Duluth Gabbro” (Takehara et al., 2018) [1]. Zircons from these two rock samples are widely used as reference materials for U–Pb dating by micro-beam techniques. Rock samples with nearly equal weights were pulverized by both methods, and the recovered zircon grains were then concentrated using conventional mineral-separation methods. Weights of the products at each step in the mineral separation process were measured, and finally the recovery rates of the heavy and non-magnetic minerals, including zircon, were calculated.
AB - In this data article, we provide information on the recovery rate and scanning electron microscope (SEM) images of the external morphology of zircon grains separated from two rock samples (AS3 and TEMORA 2) using both mechanical and electrical pulverization systems. The data in this article are related to the research article entitled “New insight into disturbance of U-Pb and trace-element systems in hydrothermally altered zircon via SHRIMP analyses of zircon from the Duluth Gabbro” (Takehara et al., 2018) [1]. Zircons from these two rock samples are widely used as reference materials for U–Pb dating by micro-beam techniques. Rock samples with nearly equal weights were pulverized by both methods, and the recovered zircon grains were then concentrated using conventional mineral-separation methods. Weights of the products at each step in the mineral separation process were measured, and finally the recovery rates of the heavy and non-magnetic minerals, including zircon, were calculated.
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U2 - 10.1016/j.dib.2018.06.016
DO - 10.1016/j.dib.2018.06.016
M3 - Article
AN - SCOPUS:85049334772
SN - 2352-3409
VL - 19
SP - 1537
EP - 1544
JO - Data in Brief
JF - Data in Brief
ER -