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Present geothermal field of the Santos Basin, Brazil

The Santos Basin, located in the southeastern waters of Brazil, is a passive continental margin basin with the most abundant deepwater petroleum resources in the world discovered to date. However, few studies have been conducted on the present geothermal fields of the Santos Basin, which severely re...

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Autores principales: Zuo, Guoping, Wang, Hongping, Lan, Lei, Zhang, Yonggang, Zuo, Yinhui, Yang, Liu, Wang, Chaofeng, Pang, Xu, Song, Xu, Yang, Meihua
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10390514/
https://www.ncbi.nlm.nih.gov/pubmed/37524761
http://dx.doi.org/10.1038/s41598-023-39702-5
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author Zuo, Guoping
Wang, Hongping
Lan, Lei
Zhang, Yonggang
Zuo, Yinhui
Yang, Liu
Wang, Chaofeng
Pang, Xu
Song, Xu
Yang, Meihua
author_facet Zuo, Guoping
Wang, Hongping
Lan, Lei
Zhang, Yonggang
Zuo, Yinhui
Yang, Liu
Wang, Chaofeng
Pang, Xu
Song, Xu
Yang, Meihua
author_sort Zuo, Guoping
collection PubMed
description The Santos Basin, located in the southeastern waters of Brazil, is a passive continental margin basin with the most abundant deepwater petroleum resources in the world discovered to date. However, few studies have been conducted on the present geothermal fields of the Santos Basin, which severely restricts the oil and gas resource evaluation of the basin. This study first utilizes 35 temperature data from 16 post-salt drilling wells and 370 temperature data from 31 pre-salt drilling wells to calculate the post-salt and pre-salt geothermal gradients and terrestrial heat flows in the Santos Basin. Then, the basin simulation software BasinMod 1D is used to quantitatively evaluate the impacts of salt rock sedimentation on the present geothermal fields and the maturity of pre-salt hydrocarbon source rocks. The results demonstrate that the present post-salt geothermal gradient in the Santos Basin is 2.20–3.97 °C/100 m, with an average value of 2.99 °C /100 m, and the post-salt terrestrial heat flow is 54.00–97.32 mW/m(2), with an average value of 73.36 mW/m(2), while the present pre-salt geothermal gradient is 2.21–2.95 °C/100 m, with an average value of 2.53 °C/100 m, and the pre-salt terrestrial heat flow is 61.85–82.59 mW/m(2), with an average value of 70.69 mW/m(2). These values are characteristic of a low-temperature geothermal field in a zone with a stable structure. The sedimentation of the salt rock causes a decrease in the temperature of the pre-salt strata, which inhibits pre-salt hydrocarbon source rock maturity, with an inhibition rate of up to 1.32%. The inhibition degree decreases with increasing salt rock thickness. At the same time, the salt rock thickness is positively correlated with the present surface heat flow. The unique distribution of the salt rock and related salt structures lead to present terrestrial heat flow differences among different structural units in the basin. This study is of great significance for evaluating and exploring the pre-salt oil and gas resources in the Santos Basin.
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spelling pubmed-103905142023-08-02 Present geothermal field of the Santos Basin, Brazil Zuo, Guoping Wang, Hongping Lan, Lei Zhang, Yonggang Zuo, Yinhui Yang, Liu Wang, Chaofeng Pang, Xu Song, Xu Yang, Meihua Sci Rep Article The Santos Basin, located in the southeastern waters of Brazil, is a passive continental margin basin with the most abundant deepwater petroleum resources in the world discovered to date. However, few studies have been conducted on the present geothermal fields of the Santos Basin, which severely restricts the oil and gas resource evaluation of the basin. This study first utilizes 35 temperature data from 16 post-salt drilling wells and 370 temperature data from 31 pre-salt drilling wells to calculate the post-salt and pre-salt geothermal gradients and terrestrial heat flows in the Santos Basin. Then, the basin simulation software BasinMod 1D is used to quantitatively evaluate the impacts of salt rock sedimentation on the present geothermal fields and the maturity of pre-salt hydrocarbon source rocks. The results demonstrate that the present post-salt geothermal gradient in the Santos Basin is 2.20–3.97 °C/100 m, with an average value of 2.99 °C /100 m, and the post-salt terrestrial heat flow is 54.00–97.32 mW/m(2), with an average value of 73.36 mW/m(2), while the present pre-salt geothermal gradient is 2.21–2.95 °C/100 m, with an average value of 2.53 °C/100 m, and the pre-salt terrestrial heat flow is 61.85–82.59 mW/m(2), with an average value of 70.69 mW/m(2). These values are characteristic of a low-temperature geothermal field in a zone with a stable structure. The sedimentation of the salt rock causes a decrease in the temperature of the pre-salt strata, which inhibits pre-salt hydrocarbon source rock maturity, with an inhibition rate of up to 1.32%. The inhibition degree decreases with increasing salt rock thickness. At the same time, the salt rock thickness is positively correlated with the present surface heat flow. The unique distribution of the salt rock and related salt structures lead to present terrestrial heat flow differences among different structural units in the basin. This study is of great significance for evaluating and exploring the pre-salt oil and gas resources in the Santos Basin. Nature Publishing Group UK 2023-07-31 /pmc/articles/PMC10390514/ /pubmed/37524761 http://dx.doi.org/10.1038/s41598-023-39702-5 Text en © The Author(s) 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Zuo, Guoping
Wang, Hongping
Lan, Lei
Zhang, Yonggang
Zuo, Yinhui
Yang, Liu
Wang, Chaofeng
Pang, Xu
Song, Xu
Yang, Meihua
Present geothermal field of the Santos Basin, Brazil
title Present geothermal field of the Santos Basin, Brazil
title_full Present geothermal field of the Santos Basin, Brazil
title_fullStr Present geothermal field of the Santos Basin, Brazil
title_full_unstemmed Present geothermal field of the Santos Basin, Brazil
title_short Present geothermal field of the Santos Basin, Brazil
title_sort present geothermal field of the santos basin, brazil
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10390514/
https://www.ncbi.nlm.nih.gov/pubmed/37524761
http://dx.doi.org/10.1038/s41598-023-39702-5
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