| 冷泉流体沉积碳酸盐岩的地质地球化学特征 |
| |
| 引用本文： | 陈多福,陈先沛,陈光谦.冷泉流体沉积碳酸盐岩的地质地球化学特征[J].沉积学报,2002,20(1):34-40. |
| |
| 作者姓名： | 陈多福 陈先沛 陈光谦 |
| |
| 作者单位： | 中国科学院广州地球化学研究所 广州五山 510640 |
| |
| 基金项目： | 国家自然科学基金，科技部基础司资助项目，40072044，，， |
| |
| 摘 要： | 冷泉流体是指来自海底沉积界面之下的低温流体以喷涌和渗漏方式注入盆地, 并产生系列的物理和化学及生物作用, 这种作用及产物称为冷泉?它是继洋中脊以盆下源中高温流体的热泉被发现和研究之后的又一个新的盆地流体沉积领域?日前研究较多的是以水? 碳氢化合物 (天然气和石油) ? 硫化氢? 细粒沉积物为主要成分, 温度与海水相近的流体, 广泛发育于活动和被动大陆边缘斜坡海底?冷泉流体沉积体系发育高密度的化学自养生物群, 以碳酸盐岩和天然气水合物为主, 有少量的硫化物和硫酸盐等?冷泉碳酸盐岩的产状有丘? 结核? 硬底? 烟囱? 胶结物和小脉等, 以化学自养生物碎屑和多期次的自生碳酸盐胶结物组成的生物丘最为常见, 它在物质来源? 形成环境? 形成作用等方面与传统来源于海水碳的碳酸盐岩建隆不同, 用术语 C h e r m o h e r m 表示, 以区别于传统海水碳酸盐岩建隆术语b i o h e r m s ? l i t h o h e r m s ? p s e u d o b i o h e r m s 和 b i o s t r o m e s ?地层中石化的化学自养生物丘常是含有大量底栖生物化石的碳酸盐岩建隆产于深水相沉积地层中, 在沉积环境和相分析上出现纵向和横向的不连续, 甚至出现反常现象?矿物以镁方解石? 白云石和文石为主, 与传统的碳酸盐岩相似, 在地球化学组成上最大的区别是冷泉流体沉积碳酸盐岩的碳来源于冷泉体系中的细菌生物成因碳, 具有特别负的碳同位素值?冷泉在海底主要沿构造带和高渗透地层呈线性群, 或围绕泥火山或盐底劈顶部呈圆形或不规则状冷泉群分布,或以海底地形低凹处和峡谷转向处呈孤立冷泉形式产出?冷泉流体以沉积建造流体为主?上覆快速堆积? 成岩压实和胶结作用? 构造挤压和变形作用? 深部的后生作用和成岩作用? 海底沉积物中的天然气水合物分解作用是建造流体向上运移进入海底成为冷泉的驱动力?冷泉碳酸盐岩的沉积作用主要有胶结作用? 充填作用和生物化学沉积作用?冷泉流体中的碳主要是以甲烷为主的碳氢化合物形式存在, 经微生物作用转变为 C O2 ,最终形成冷泉碳酸盐岩?
|
| 关 键 词： | 冷泉流体沉积 化学自养生物碳酸盐岩和生物丘 地质和地球化学特征 |
| 文章编号： | 1000-0550(2002)01-0034-07 |
| 收稿时间： | 2001-04-20 |
| 修稿时间： | 2001年4月20日 |
Geology and Geochemistry of Cold Seepage and Venting-related Carbonates |
| |
| CHEN Duo-fu CHEN Xian-pei CHEN Guang-qian Guangzhou Institute of Geochemistry,Chinese Academy of Sciences Guangzhou.Geology and Geochemistry of Cold Seepage and Venting-related Carbonates[J].Acta Sedimentologica Sinica,2002,20(1):34-40. |
| |
| Authors: | CHEN Duo-fu CHEN Xian-pei CHEN Guang-qian Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou |
| |
| Institution: | Guangzhou,Institute of Geochemistry, Chinese Academy of Sciences Guangzhou 510640 |
| |
| Abstract: | Cold seepage and venting is a fluid seepage and venting mainly composed of water, hydrocarbon(gas and crude oil), hydrogen sulfide and fine sediments derived below seafloor. Its temperature is similar to sea water and widely occurs on the seafloor of continental slope of active and passive margins. Cold seepage and venting-related chemosynthetic communities are highly in organism density, mainly mussels, clams, tube worms and bacterial mats. The sediments in cold seepage and venting are mostly maed up of carbonates and gas hydrates with minor sulfides and sulphates. The chemosynthetic carbonates occurred as buildup, chimney, cement, nodule, hardgroud and fine vein, and generally as buildup of chemosythetic bioclasts and multi-stage authigenic cements. The carbonate source, sedimentary environment and sedimentations are different with normal carbonates,of which carbon is from sea water. Therefore, using term "Chermoherm" represents the chemosynthetic carbonate buildup to distinguish from the terms of bioherms, lithoherms, pseudobioherms, biostromes of carbonate buildups in normal sea environment,in which the carbon is from sea water. In strata, Chermoherm frequently occurred in abyssal sediment strata as a carbonate buildup containing a lot of fossils of benthic fauna. There are disrupted sedimentary phase and environments in longitudinal and cross strata section, so much as turnover. Carbonate minerals in chemosynthetic carbonates are primarily Mg-calcite, aragonite, and dolomite,which are not different with normal carbonates. Carbon isotope values in chemosynthetic carbonates are very low due to bacteria mediation. Cold seepage and venting occurred along fault zone or permeable beds and at the surface expression of mud volcano and salt diapirism. Cold seepage and venting fluids are derived from formation fluids driven by a combination of (1)pore-space reduction of rapid sedimentation and tectonic compaction, deformation and cementation, and (2)increased buoyancy due to a decrease in pore-fluid density related diagenesis and catagenesis, and gas hydrate decomposition at depth. The sedimentation processes of cold seepage and venting-related carbonates are cementation, filling action and biochemical sedimentation. The hydrocarbon mainly of methane into cold seepage and venting is changed to carbon dioxide by bacteria mediation and deposited chemosynthetic carbonates. |
| |
| Keywords: | sediments of cold seepage and venting chemosynthetic carbonates and chemoherm geological and geochemical features |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《沉积学报》浏览原始摘要信息 |
| 点击此处可从《沉积学报》下载免费的PDF全文 |
|
