皖南埃迪卡拉系蓝田组页岩的有机质富集与孔隙发育特征
Characteristics of organic matter enrichment and pore development of the Ediacaran Lantian Formation shales from southern Anhui Province
查看参考文献29篇
文摘
|
中国南方广泛分布的三套海相黑色页岩中,埃迪卡拉系页岩的有机质分布与富集特征研究较为薄弱。在皖南蓝田组黑色页岩近期的研究基础上,进一步对比分析了扬子区不同沉积相页岩的有机质富集规律,通过不同显微尺度的观察技术研究了蓝田组页岩中有机质的分布特征,并根据扫描电镜观察结果采用图像分析方法评价了孔隙发育特征。结果表明:(1)埃迪卡拉系有机质富集层位主要有3套,以下扬子皖南地区沉积的蓝田组(相当于陡山沱组)Ⅱ段为最优;(2)蓝田组页岩中有机质多以不规则多边形、条带或基质分散的形式充填于矿物粒间、黄铁矿晶间以及黏土矿物集合体层间,大量的黄铁矿主要以<10μm的草莓状集合体形式出现,晶体间几乎全部被有机质充填;(3)高分辨扫描电镜图像分析表明,蓝田组页岩的孔隙以有机孔为主,孔径多小于100 nm。 |
其他语种文摘
|
Among the three main sets of marine black shales widespread in South China, the Ediacaran shales have attracted little attention concerning the distribution and enrichment of organic matter (OM). Based on recent investigations on black shales from the Lantian Formation in southern Anhui Province, the characteristics of OM enrichment for shales from various sedimentary facies of the Yangtze Block are compared and primarily summarized. The OM distribution in the Lantian Formation shales is illustrated through different scales of observation techniques, and pore characteristics are acquired through SEM image analysis. Comparison with several published results indicates that Member II of the Lantian Formation (equivalent to the Doushantuo Formation) deposited in the slope setting of southern Anhui Province is the best among three major layers with respect to OM enrichment during the Ediacaran period. OM from the Lantian Formation shales shows irregular polygon-, belt- and matrix-like shapes and largely fills among mineral particles, pyrite crystals and interlayers of clay aggregates. Pyrites exist mainly in the form of framboids smaller than 10 μm, and their intercrystal voids are almost completely filled with OM. High-resolution SEM images also suggest that the pore system of the Lantian Formation shales is dominated by organic pores (pore size mostly smaller than 100 nm). |
来源
|
地球化学
,2017,46(2):158-167 【核心库】
|
关键词
|
埃迪卡拉系
;
蓝田组页岩
;
有机质
;
黄铁矿
;
孔隙
|
地址
|
1.
中国科学院广州地球化学研究所, 有机地球化学国家重点实验室, 广东, 广州, 510640
2.
中国科学院南京地质古生物研究所, 中国科学院资源地层学与古地理学重点实验室, 江苏, 南京, 210008
3.
中国科学院南京地质古生物研究所, 现代古生物学和地层学国家重点实验室, 江苏, 南京, 210008
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
0379-1726 |
学科
|
地质学 |
基金
|
中国科学院重点部署项目
;
中国科学院战略性先导科技专项
;
中国科学院“一三五”规划
|
文献收藏号
|
CSCD:5968199
|
参考文献 共
29
共2页
|
1.
邹才能. 中国页岩气形成条件及勘探实践.
天然气工业,2011,31(12):26-39
|
CSCD被引
143
次
|
|
|
|
2.
董大忠. 论四川盆地页岩气资源勘探开发前景.
天然气工业,2014,34(12):1-15
|
CSCD被引
138
次
|
|
|
|
3.
Tan J Q. Shale gas potential of the major marine shale formations in the Upper Yangtze Platform, South China, Part III: Mineralogical, lithofacial, petrophysical, and rock mechanical properties.
Energ Fuel,2014,28(4):2322-2342
|
CSCD被引
16
次
|
|
|
|
4.
McFadden K A. Pulsed oxidation and bioloical evolution in the Ediacaran Doushantuo Formation.
Proc Natl Acad Sci USA,2008,105(9):3197-3202
|
CSCD被引
107
次
|
|
|
|
5.
Li C. A stratified redox model for the Ediacaran Ocean.
Science,2010,328(5974):80-83
|
CSCD被引
106
次
|
|
|
|
6.
Yuan X L. An early Ediacaran assemblage of macroscopic and morphologically differentiated eukaryotes.
Nature,2011,470(7334):390-393
|
CSCD被引
45
次
|
|
|
|
7.
袁训来. 蓝田生物群:一个认识多细胞生物起源和早期演化的新窗口.
科学通报,2012,57(34):3219-3227
|
CSCD被引
6
次
|
|
|
|
8.
Guan C G. Fluctuation of shelf basin redox conditions in the early Ediacaran: Evidence from Lantian Formation black shales in South China.
Precamb Res,2014,245:1-12
|
CSCD被引
6
次
|
|
|
|
9.
Zeng J. Composition and pore characteristics of black shales from the Ediacaran Lantian Formation in the Yangtze Block, South China.
Mar Pet Geol,2016,76:246-261
|
CSCD被引
4
次
|
|
|
|
10.
Guo Q J. Carbon isotopic evolution of the terminal neoproterozoic and early Cambrian: Evidence from the Yangtze platform, South China.
Palaeogeogr Palaeocl,2007,254(1/2):140-157
|
CSCD被引
28
次
|
|
|
|
11.
Jiang G Q. Organic carbon isotope constraints on the dissolved organic carbon (DOC) reservoirat the Cryogenian-Ediacaran transition.
Earth Planet Sci Lett,2010,299:159-168
|
CSCD被引
7
次
|
|
|
|
12.
Zhu M Y. Integrated Ediacaran (Sinian) chronostratigraphy of South China.
Palaeogeogr Palaeocl,2007,254(1/2):7-61
|
CSCD被引
73
次
|
|
|
|
13.
National Institutes of Health, USA.
Image J
|
CSCD被引
1
次
|
|
|
|
14.
王金权. 皖南震旦系蓝田组沉积岩有机碳同位素记录.
古生物学报,2004,43(3):424-432
|
CSCD被引
7
次
|
|
|
|
15.
魏国齐. 四川盆地震旦系大气田形成条件与勘探远景区.
石油勘探与开发,2013,40(2):129-138
|
CSCD被引
72
次
|
|
|
|
16.
Fike D A. Oxidation of the Ediacaran Ocean.
Nature,2006,444(7120):744-747
|
CSCD被引
120
次
|
|
|
|
17.
Lee C. Carbon isotopes and lipid biomarkers from organic-richfacies of the Shuram Formation, Sultanate of Oman.
Geobiology,2013,11:406-419
|
CSCD被引
4
次
|
|
|
|
18.
Canfield D E. Factors influencing organic carbon preservation in marine sediments.
Chem Geol,1994,114:315-329
|
CSCD被引
44
次
|
|
|
|
19.
Kennedy M. Late Precambrian oxygenation: Inception of the clay mineral factory.
Science,2006,311(5766):1446-1449
|
CSCD被引
20
次
|
|
|
|
20.
Fishman N S. The nature of porosity in organic-rich mudstones of the Upper Jurassic Kimmeridge Clay Formation, North Sea, offshore United Kingdom.
Int J Coal Geol,2012,103:32-50
|
CSCD被引
52
次
|
|
|
|
|