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CORRECTION article

Front. Earth Sci., 23 May 2023
Sec. Structural Geology and Tectonics
Volume 11 - 2023 | https://doi.org/10.3389/feart.2023.1201571

Corrigendum: Diagenesis of the first member of Canglangpu formation of the Cambrian Series 2 in northern part of the central Sichuan Basin and its influence on porosity

www.frontiersin.orgBing Zou1,2 www.frontiersin.orgHaizhou Qu1,2* www.frontiersin.orgRongrong Zhao3 www.frontiersin.orgLianjin Zhang4 www.frontiersin.orgYu Zhang3 www.frontiersin.orgZike Ma4 www.frontiersin.orgXingyu Zhang1 www.frontiersin.orgQinyang Huang1,2 www.frontiersin.orgQianwen Mo3 www.frontiersin.orgHongyi An3 www.frontiersin.orgYu Pei5
  • 1State Key Laboratory of Oil and Gas Reservoir Geology and Development Engineering, Southwest Petroleum University, Chengdu, China
  • 2School of Geoscience and Technology, Southwest Petroleum University, Chengdu, China
  • 3Exploration department of Petrochina Southwest Oil and Gasfield Company, Chengdu, China
  • 4Central Sichuan Oil and Gas Mine of PetroChina Southwest Oil and Gas Field Company, Suining, China
  • 5Geological Exploration & Development Research Institute, CNPC Chuanqing Drilling Engineering Company Limited, Chengdu, China

An Corrigendum on
Diagenesis of the first member of Canglangpu Formation of the Cambrian Terreneuvian in northern part of the central Sichuan Basin and its influence on porosity

by Zhou B, Qu H, Zhao R, Zhang L, Zhang Y, Ma Z, Zhang X, Huang Q, Mo Q, An H and Pei Y (2023). Front. Earth Sci. 10:1059838. doi: 10.3389/feart.2022.1059838

In the published article, there was an error in the article title. Instead of “Diagenesis of the first member of Canglangpu Formation of the Cambrian Terreneuvian in northern part of the central Sichuan Basin and its influence on porosity”, it should be “Diagenesis of the first member of Canglangpu Formation of the Cambrian Series 2 in northern part of the central Sichuan Basin and its influence on porosity”.

In the published article, there was an error in Figure 1 as published. In the picture, the age of the strata is incorrect. The corrected Figure 1 and its caption appear below.

FIGURE 1
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FIGURE 1. Location and comprehensive stratigraphic histogram of the study area. (A) Structural unit division of the Sichuan Basin (modified from Reference Hu (2021)); (B) Lithologic histogram of the Canglangpu Formation in Well CT1. GR: natural gamma ray; Rt: true formation resistivity; Rxo: flushed zone formation resistivity.

In the published article, there was an error in Table 2 as published. The stratigraphic age in the table name is incorrect. The corrected Table 2 and its caption appear below.

TABLE 2
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TABLE 2. Contents of carbon and oxygen isotopes in the first member of Canglangpu Formation of the Cambrian Series 2 in well JT1, central Sichuan Basin (Ma at el., 2022).

In the published article, there was an error in Table 3 as published. The stratigraphic age in the table name is incorrect. The corrected Table 3 and its caption appear below.

TABLE 3
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TABLE 3. Date of paleotemperature and paleo-salinity of the first member of Canglangpu Formation of the Cambrian Series 2 from Well JT1 in central Sichuan Basin (Ma at el., 2022).

In the published article, there was an error in Figure 7 as published. In the picture, the age of the strata is incorrect. The corrected Figure 7 and its caption appear below.

FIGURE 7
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FIGURE 7. Histogram of diagenesis in coring section of well CT1.

In the published article, there was an error. The stratigraphic age is incorrectly divided. A correction has been made to the Abstract, paragraph 1. The corrected sentence appears below:

“In this paper, taking the first Member of the Canglangpu Formation of the Cambrian Series 2 in the northern central Sichuan Basin as an example.”

A correction has been made to the keywords. The corrected keywords appear below:

“diagenesis, Series 2, Cambrian, the first member of Canglangpu Formation, northern part of the Central Sichuan Basin”

A correction has been made to the Introduction, paragraph 1. The corrected sentence appears below:

“The Central Sichuan Paleo-uplift controls the process of hydrocarbon accumulation in the Sinian-Cambrian Series 2 in the Sichuan Basin. At present, the exploration horizons in this area are mainly concentrated in the Sinian Dengying Formation and the Cambrian Series 2 Longwangmiao Formation, and there are few studies on other horizons.”

A correction has been made to the Conclusion, paragraph 1. The corrected sentence appears below:

“In this paper, taking the Cang 1 Member of the Canglangpu Formation of the Cambrian Series 2 in the north part of the central Sichuan Basin as an example.”

The authors apologize for these errors and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.

Publisher’s note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

Keywords: diagenesis, Series 2, Cambrian, the first member of Canglangpu formation, northern part of the central Sichuan Basin

Citation: Zou B, Qu H, Zhao R, Zhang L, Zhang Y, Ma Z, Zhang X, Huang Q, Mo Q, An H and Pei Y (2023) Corrigendum: Diagenesis of the first member of Canglangpu formation of the Cambrian Series 2 in northern part of the central Sichuan Basin and its influence on porosity. Front. Earth Sci. 11:1201571. doi: 10.3389/feart.2023.1201571

Received: 06 April 2023; Accepted: 16 May 2023;
Published: 23 May 2023.

Edited and reviewed by:

Derek Keir, University of Southampton, United Kingdom

Copyright © 2023 Zou, Qu, Zhao, Zhang, Zhang, Ma, Zhang, Huang, Mo, An and Pei. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Haizhou Qu, quhaizhou@swpu.edu.cn

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