Characterizing a complex buildup in the Pearl River Mouth Basin of the northern South China Sea: an interplay of carbonates and igneous rocks

Volcanic mounds and carbonate buildups share similar geometries, making their differentiation in seismic data a significant challenge. This challenge is further compounded in complex buildups composed of both multi-stage developed igneous rocks and biogenic carbonates. To address this gap, this stud...

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Main Authors: Beichen Chen, Leyi Xu, Baojun Liu, Lili Zhang, Dong Xiao, Ya Gao, Feng Wu, Xueqi Yang, Yaming Zou, Yongkun Ma, Yinglin Zhang
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-01-01
Series:Frontiers in Marine Science
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Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2024.1518292/full
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author Beichen Chen
Leyi Xu
Baojun Liu
Lili Zhang
Dong Xiao
Ya Gao
Ya Gao
Feng Wu
Xueqi Yang
Yaming Zou
Yongkun Ma
Yinglin Zhang
author_facet Beichen Chen
Leyi Xu
Baojun Liu
Lili Zhang
Dong Xiao
Ya Gao
Ya Gao
Feng Wu
Xueqi Yang
Yaming Zou
Yongkun Ma
Yinglin Zhang
author_sort Beichen Chen
collection DOAJ
description Volcanic mounds and carbonate buildups share similar geometries, making their differentiation in seismic data a significant challenge. This challenge is further compounded in complex buildups composed of both multi-stage developed igneous rocks and biogenic carbonates. To address this gap, this study investigates a mixed carbonate-igneous buildup at the central of the Baiyun Sag in the northern South China Sea. By analyzing the lithofacies of the carbonates and igneous rocks, the morphological features and spatial distribution patterns corresponding to these sedimentary and volcanic facies were identified. Well-to-seismic calibration was used to delineate the stratigraphic units, and typical seismic profiles of the buildup were analyzed. Eight distinct seismic facies were identified for carbonates and igneous rocks. The evolution of the buildup is divided into three stages: (1) volcanic eruptions and carbonates development, (2) overflowing magma and reef shoal deposits, and (3) reef-bank deposition accompanied by igneous intrusion. We propose that volcanic rocks can be distinguished from carbonates by the temporal and spatial coupling of typical features: (a) surface volcanic rocks and subsurface intrusive bodies are inseparable, with igneous rocks identifiable through faults and volcanic conduits; (b) carbonates typically display symmetrical structures on both sides of the highland and exhibit better stratification away from igneous activity; (c) carbonates generally show a convex clinoform and steep slope at the platform margin, while volcanic mounds exhibit concave gentle slopes. Furthermore, the analysis of high-quality reservoir development within the complex buildups is instrumental for advancing oil and gas exploration in volcanic seamounts and carbonate buildups.
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spelling doaj-art-dba522a1a5f946f4a18bc5011838d0042025-01-28T08:36:35ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452025-01-011110.3389/fmars.2024.15182921518292Characterizing a complex buildup in the Pearl River Mouth Basin of the northern South China Sea: an interplay of carbonates and igneous rocksBeichen Chen0Leyi Xu1Baojun Liu2Lili Zhang3Dong Xiao4Ya Gao5Ya Gao6Feng Wu7Xueqi Yang8Yaming Zou9Yongkun Ma10Yinglin Zhang11Research Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaResearch Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaResearch Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaResearch Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaResearch Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaSchool of Marine Sciences, Sun Yat-sen University, Zhuhai, ChinaHubei Key Laboratory of Marine Geological Resources, China University of Geosciences (CUG), Wuhan, ChinaCollege of Oceanography, Hohai University, Nanjing, ChinaResearch Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaResearch Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaResearch Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaResearch Institute, Shenzhen Branch of China National Offshore Oil Corporation Ltd., Shenzhen, ChinaVolcanic mounds and carbonate buildups share similar geometries, making their differentiation in seismic data a significant challenge. This challenge is further compounded in complex buildups composed of both multi-stage developed igneous rocks and biogenic carbonates. To address this gap, this study investigates a mixed carbonate-igneous buildup at the central of the Baiyun Sag in the northern South China Sea. By analyzing the lithofacies of the carbonates and igneous rocks, the morphological features and spatial distribution patterns corresponding to these sedimentary and volcanic facies were identified. Well-to-seismic calibration was used to delineate the stratigraphic units, and typical seismic profiles of the buildup were analyzed. Eight distinct seismic facies were identified for carbonates and igneous rocks. The evolution of the buildup is divided into three stages: (1) volcanic eruptions and carbonates development, (2) overflowing magma and reef shoal deposits, and (3) reef-bank deposition accompanied by igneous intrusion. We propose that volcanic rocks can be distinguished from carbonates by the temporal and spatial coupling of typical features: (a) surface volcanic rocks and subsurface intrusive bodies are inseparable, with igneous rocks identifiable through faults and volcanic conduits; (b) carbonates typically display symmetrical structures on both sides of the highland and exhibit better stratification away from igneous activity; (c) carbonates generally show a convex clinoform and steep slope at the platform margin, while volcanic mounds exhibit concave gentle slopes. Furthermore, the analysis of high-quality reservoir development within the complex buildups is instrumental for advancing oil and gas exploration in volcanic seamounts and carbonate buildups.https://www.frontiersin.org/articles/10.3389/fmars.2024.1518292/fullcarbonate platformvolcanic moundseismic faciesplatform evolutionthe baiyun sag
spellingShingle Beichen Chen
Leyi Xu
Baojun Liu
Lili Zhang
Dong Xiao
Ya Gao
Ya Gao
Feng Wu
Xueqi Yang
Yaming Zou
Yongkun Ma
Yinglin Zhang
Characterizing a complex buildup in the Pearl River Mouth Basin of the northern South China Sea: an interplay of carbonates and igneous rocks
Frontiers in Marine Science
carbonate platform
volcanic mound
seismic facies
platform evolution
the baiyun sag
title Characterizing a complex buildup in the Pearl River Mouth Basin of the northern South China Sea: an interplay of carbonates and igneous rocks
title_full Characterizing a complex buildup in the Pearl River Mouth Basin of the northern South China Sea: an interplay of carbonates and igneous rocks
title_fullStr Characterizing a complex buildup in the Pearl River Mouth Basin of the northern South China Sea: an interplay of carbonates and igneous rocks
title_full_unstemmed Characterizing a complex buildup in the Pearl River Mouth Basin of the northern South China Sea: an interplay of carbonates and igneous rocks
title_short Characterizing a complex buildup in the Pearl River Mouth Basin of the northern South China Sea: an interplay of carbonates and igneous rocks
title_sort characterizing a complex buildup in the pearl river mouth basin of the northern south china sea an interplay of carbonates and igneous rocks
topic carbonate platform
volcanic mound
seismic facies
platform evolution
the baiyun sag
url https://www.frontiersin.org/articles/10.3389/fmars.2024.1518292/full
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