中国近海新生代优质烃源岩富营养化机制与油气潜力综述

Journal of Natural Gas Geoscience Pub Date : 2026-08-01 Epub Date: 2026-07-28 DOI:10.1016/j.jnggs.2026.07.001
Dujie Hou, Jiahao He, Qian Huang, Yingzhong Zhu, Rui Hu, Wei Si, Hai Liu, Xiong Cheng, Lin Wei
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摘要

中国近海优质烃源岩的发育与富营养化密切相关,富营养化为生烃提供了重要的基础。本文分析了中国近海湖相和海相优质烃源岩的成因,重点讨论了6种主要的富营养化机制:热液施肥、火山施肥、花岗岩风化耦合河流搬运、中度盐渍化、封闭至半封闭海湾和上升流。这些机制通过向水生环境提供丰富的营养物质(如P、Fe、Mn、Zn、N和Si)或创造有利的环境条件(如低能水动力环境、缺氧条件和中等盐度),促进浮游生物特别是藻类的大量繁殖,从而为富有机质烃源岩的发育提供物质基础。前人的研究表明,中国近海广泛发育的湖相优质烃源岩(如渤海湾盆地的沙河街组、珠江口盆地的文昌组、北部湾盆地的六沙岗组)是在强烈裂陷过程中形成的半深至深湖相环境中发育的,同时还伴有富营养的热液活动、火山活动、海相沉积等。陆源输入促进了优势藻类群落的增殖。而海相优质烃源岩(如琼东南盆地崖城组)的形成则与封闭至半封闭海湾的营养物聚集和上升流向上搬运营养物密切相关。这些环境条件促进了水生生物的繁盛,提高了烃源岩的质量。本文强调了富营养化对油气潜力的控制作用,为认识近海含油气盆地优质烃源岩的发育提供了理论依据,并对巨型气田、生物气和天然气水合物的形成提供了新的认识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Eutrophication mechanisms and hydrocarbon potential of Cenozoic excellent source rocks in offshore China: A critical review
Development of excellent source rocks in offshore China is closely associated with eutrophication, which provides an important foundation for the hydrocarbon generation. This review analyzes the origins of lacustrine and marine excellent source rocks in offshore China, focusing on six major eutrophication mechanisms: hydrothermal fertilization, volcanic fertilization, granite weathering coupled with fluvial transport, moderate salinization, closed to semi-closed bays, and upwelling currents. These mechanisms promote plankton blooms, particularly those of algae, by supplying abundant nutrients (e.g., P, Fe, Mn, Zn, N, and Si) to aquatic environments or by creating favorable environmental conditions (e.g., low-energy hydrodynamic settings, anoxic conditions, and moderate salinity), thereby providing the material basis for the development of organic-rich source rocks. Previous studies indicate that the widely developed lacustrine excellent source rocks in offshore China (e.g., the Shahejie Formation in the Bohai Bay Basin, the Wenchang Formation in the Pearl River Mouth Basin, and the Liushagang Formation in the Beibu Gulf Basin) developed in semi-deep to deep lacustrine environments formed during intense rifting, together with nutrient-rich hydrothermal activity, volcanic activity, and terrigenous inputs that facilitated the proliferation of dominant algal communities. In contrast, the formation of marine excellent source rocks (e.g., the Yacheng Formation in the Qiongdongnan Basin) is closely related to nutrient accumulation in closed to semi-closed bays and the upward transport of nutrients by upwelling currents. These environmental conditions promoted the flourishing of aquatic organisms and enhanced the quality of source rocks. This review highlights the influence of eutrophication in controlling hydrocarbon potential, providing a theoretical basis for understanding the development of excellent source rocks in offshore petroliferous basins and offering new insights into the formation of giant gas fields, biogenic gas, and natural gas hydrates.
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