The patent badge is an abbreviated version of the USPTO patent document. The patent badge does contain a link to the full patent document.

The patent badge is an abbreviated version of the USPTO patent document. The patent badge covers the following: Patent number, Date patent was issued, Date patent was filed, Title of the patent, Applicant, Inventor, Assignee, Attorney firm, Primary examiner, Assistant examiner, CPCs, and Abstract. The patent badge does contain a link to the full patent document (in Adobe Acrobat format, aka pdf). To download or print any patent click here.

Date of Patent:
Aug. 05, 2025

Filed:

Aug. 18, 2023
Applicants:

Zijin Mining Group Co., Ltd., Longyan, CN;

China University of Geosciences (Wuhan), Wuhan, CN;

Inventors:

Youye Zheng, Wuhan, CN;

Shouhong Lin, Wuhan, CN;

Changshun Jia, Wuhan, CN;

Xiaodan Lai, Wuhan, CN;

Xu Kang, Wuhan, CN;

Jinzhang Zhang, Wuhan, CN;

Rongzhu Guan, Wuhan, CN;

Xiaojia Jiang, Wuhan, CN;

Xin Chen, Wuhan, CN;

Attorneys:
Primary Examiner:
Int. Cl.
CPC ...
G01N 27/62 (2021.01); G01N 33/24 (2006.01);
U.S. Cl.
CPC ...
G01N 27/62 (2013.01); G01N 33/24 (2013.01); G01N 2223/01 (2013.01); G01N 2223/073 (2013.01);
Abstract

In a method for in-situ U-Pb dating of heterogeneous minerals, a target mineral is separated and purified by carrying out data analysis, extraction and enhancement on original mapping data. The method highlights distribution features of dating indexes (U content, Pb content, Pb/Uratio, Pb/Uratio and Th/U ratio) in a target mineral phase with a noise data processing technology, and more intuitively displays a favorable dating portion and a crystal growth change trend of the dating mineral. Further, a fine spot design is provided for high-precision dating analysis in a later stage. A plurality of geological events experienced by a heterogeneous mineral crystal in a growth process is accurately limited, so as to invert the mineral formation history which provides the basis for better study of mineralogy, mineral geochemistry and mineral geochronology. It is hence a novel indispensable auxiliary means of mineral geochronology and an auxiliary method for mineral exploration.


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