塔里木盆地东河砂岩段中的生物扰动作用
Bioturbation of Donghe Sandstone Member in Tarim Basin
查看参考文献18篇
文摘
|
生物扰动作用对沉积过程的影响比较复杂,一般认为生物扰动作用发生在表层细粒泥质沉积物中,如深海海底,河口湾,潮滩等环境下.塔里木盆地东河砂岩段为高能碎屑滨岸沉积,其中含大量的遗迹化石,也发育大量的生物扰动构造,说明高能环境下存在生物扰动的事实.生物扰动强度也是进一步识别各沉积微相的依据,隐性生物扰动作用甚至可以保留原始沉积构造 |
其他语种文摘
|
The effect of bioturbation to deposition process is complex. It is generally recognized that bioturbation exists in surface granular mud sediments, such as the deep sea beds, estuary bays, tidal flats and other conditions. Donghe sandstone member in Tarim basin was deposited in high-energy shore clastic sedimentary environment. The numerous trace fossils and a large number of bioturbation structures may state the fact that there exists bioturbation in high-energy environment. The intensity of bioturbation has further become the evidence of identifying the sedimentary microfacies and the crypto-bioturbation can always reflect the original sedimentary structure |
来源
|
新疆石油地质
,2010,31(5):493-496 【核心库】
|
关键词
|
塔里木盆地
;
东河砂岩段
;
生物扰动作用
;
滨岸环境
;
沉积微相
|
地址
|
1.
中国科学院广州地球化学研究所, 广州, 510640
2.
中国石油杭州地质研究院, 杭州, 310023
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
1001-3873 |
学科
|
石油、天然气工业 |
文献收藏号
|
CSCD:4036929
|
参考文献 共
18
共1页
|
1.
顾家裕. 塔里木盆地东河砂岩沉积和储层特征及综合分析.
古地理学报,2006,8(3):285-294
|
被引
47
次
|
|
|
|
2.
郭建华. 阿克库勒凸起东河砂岩的沉积相与层序地层.
石油与天然气地质,2005,26(6):808-815
|
被引
17
次
|
|
|
|
3.
朱如凯. 塔里木盆地晚泥盆世及石炭纪岩相古地理.
古地理学报,2002,4(1):13-25
|
被引
36
次
|
|
|
|
4.
朱筱敏. 塔里木盆地塔北与塔中地区东河砂岩段沉积特征对比.
中国地质,2005,32(4):648-654
|
被引
29
次
|
|
|
|
5.
王招明. 塔里木盆地晚泥盆世一早石炭世东河砂岩沉积相.
古地理学报,2004,6(3):289-297
|
被引
41
次
|
|
|
|
6.
张惠良. 塔里木盆地东河砂岩沉积期次及油气勘探.
石油学报,2009,30(6):835-842
|
被引
29
次
|
|
|
|
7.
齐永安. 塔里木盆地晚泥盆世东河塘组河口湾相遗迹化石.
古生物学报,2003,42(2):277-283
|
被引
2
次
|
|
|
|
8.
范德江. 长江水下三角洲浅表沉积层中的生物扰动构造.
海洋与湖沼,2008,11(6):577-584
|
被引
6
次
|
|
|
|
9.
Drose M L. Ichnofabric of sandstone deposited in high energy nearshore terrigenous clastic environments: measurment and utilization.
Palaios,1989,4:598-604
|
被引
1
次
|
|
|
|
10.
de Gibert J M. Paleohydrological significance of trace fossil distribution in Oligocene fluvial-fan-tolacustrine systems of the Ebro basin, Spain.
Palaeogeography, Palaeoclimatology, Palaeoecology,2009,272:162-175
|
被引
1
次
|
|
|
|
11.
Yang B C. Sedimentation on a wave-dominated, open-coast tidal flat, southwestern Korea: summer tidal flat-winter shoreface.
Sedimentology,2005,52(2):235-252
|
被引
8
次
|
|
|
|
12.
Damholt. Laminated-bioturbated cycles in Maastrichtian chalk of the North Sea:oxygenation fluctuations within the Milankovitch frequency band.
Sedimentology,2004,51(6):1323-1342
|
被引
1
次
|
|
|
|
13.
Smith C R. Variations in bioturbation across the oxygen minimum zone in the northwest Arabian Sea.
Deep Sea Research II,2000,47:227-257
|
被引
6
次
|
|
|
|
14.
Turnewitsch R. Bioturbation in the abyssal Arabian Sea:influence of fauna and food supply.
Deep Sea Resegrch II,2000,47:2877-2911
|
被引
9
次
|
|
|
|
15.
杨群慧. 海底生物扰动作用及其对沉积过程和记录的影响.
地球科学进展,2008,23(9):932-941
|
被引
15
次
|
|
|
|
16.
Dashtgard S E. Grain-size controls on the occurrence of bioturbation.
Palaeogeography, Palaeoclimatology, Palaeoecology,257(1/2):224-243
|
被引
1
次
|
|
|
|
17.
Horbury A D. 'Pseudobreccias'revealed as calcrete mottling and bioturbation in the Late Dinantian of the southern Lake District,UK.
Sedimentology,2004,51(1):19-38
|
被引
1
次
|
|
|
|
18.
Pemberton S G. Biogenic chaos:cryptobioturbation and the work of sedimentologically friendly organism.
Palaeogeography, Palaeoclimatology, Palaeoecology,2008,270:273-279
|
被引
5
次
|
|
|
|
|