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:
Nov. 15, 2022

Filed:

Nov. 22, 2021
Applicant:

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, CN;

Inventors:

Wenyang Wang, Beijing, CN;

Yaping Wang, Beijing, CN;

Xiongqi Pang, Beijing, CN;

Zhangxing Chen, Beijing, CN;

Wang Zhang, Beijing, CN;

Rixiang Zhu, Beijing, CN;

Attorney:
Primary Examiner:
Int. Cl.
CPC ...
G01K 13/00 (2021.01); G01N 33/24 (2006.01); G06F 30/28 (2020.01); G01N 25/20 (2006.01);
U.S. Cl.
CPC ...
G01N 33/241 (2013.01); G01N 25/20 (2013.01); G06F 30/28 (2020.01); G01K 13/00 (2013.01);
Abstract

An evaluation method for residual hydrocarbon of post- to over-mature marine source rocks includes the following steps: establishing a hydrocarbon generation potential evolution profile and a hydrogen index evolution profile of post- to over-mature source rocks; determining a critical condition for hydrocarbon expulsion of the source rocks, and inverting original hydrocarbon generation potential of the source rocks; inverting a critical condition for hydrocarbon generation of the source rocks; establishing a hydrocarbon generation, expulsion and retention model for the source rocks; determining a hydrocarbon generation rate, a hydrocarbon expulsion rate and a hydrocarbon retention rate of the source rocks; and calculating a hydrocarbon retention intensity and residual hydrocarbon of the source rocks. The evaluation method establishes an evaluation model for residual hydrocarbon of post- to over-mature source rocks without relying on immature to sub-mature samples.


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