兰坪中新生代盆地沉积岩源区构造背景和物源属性研究——砂岩地球化学证据
Tectonic Setting and Provenance of Source Rock for Sedimentary Rocks in Lanping Mesozoic-Cenozoic Basin: evidences from geochemistry of sandstones
查看参考文献24篇
文摘
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沉积盆地中砂岩的地球化学成分主要受物源区控制。因此,通过分析砂岩的化学成分可以揭示盆地沉积岩的源区构造背影和物源属性。对兰坪盆地中新生界砂岩的常量成分、稀土和微量元素进行的分析,揭示盆地沉积岩的源区构造背景属被动大陆边缘和大陆岛弧,结合岩相古地理资料认为在中生代以前,盆地东侧可能主要处于被动大陆边缘环境,而西侧则可能以大陆岛弧环境为主,这与区域地质资料相吻合。沉积物源岩的原始物质应来自上地壳,以长英质岩石为主,并有少量安山质岩石和古老沉积物的混入,故兰坪中新生代盆地属典型的大陆型盆地。从而为正确认识古特提斯洋的演化和盆山转换过程提供了强有力的地球化学证据。 |
其他语种文摘
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The geochemical compositions of sandstones in sedimentary basin are controlled by the tectonic setting of source rock, and it is, therefore, possible to discriminate the tectonic setting of source rock area and provenance of source rock by studying the geochemical compositions of sandstones. The major compositions, rare earth ele-ments and trace elements of Mesozoic-Cenozoic sandstones in Lanping Basin are studied in this paper, and which reveals that the tectonic settings of source rock area for Mesozoic-Cenozoic sedimentary rocks in in Lanping Basin, belong to passive continental margin and continental island arc. Combined with the data of sedimentary facies and palaeogeography, it is referred that the east area of basin is mainly located at tectonic setting of passive continental margin before Mesozoic , whereas the west area of basin may be at continental island arc. This is compatible with the results of regional geological studied data. The primary materials of sedimentary rocks should come from the upper continental crust, and are mainly composed of felsic rocks, mixed with few andesitic rocks and old sediment components. Therefore , Lanping Mesozoic-Cenozoic Basin is the typical continental-type basin. This provides strong geochemical evidences for correctly understanding the evolution of the old Tethys and the basin-range transi-tion. |
来源
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沉积学报
,2003,21(4):547-552 【核心库】
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关键词
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砂岩
;
地球化学
;
构造背景
;
物源属性
;
兰坪中新生代盆地
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地址
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1.
中科院贵阳地球化学所, 矿床地球化学开放研究实验室, 贵阳, 550002
2.
中国地质大学(北京), 北京, 100083
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语种
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中文 |
文献类型
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研究性论文 |
ISSN
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1000-0550 |
学科
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地质学 |
基金
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国家973计划
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文献收藏号
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CSCD:1176079
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参考文献 共
24
共2页
|
1.
余谦. 云南兰坪盆地三叠纪沉积相与古地理演化.
沉积与特提斯地质,2000,20(2):33-42
|
CSCD被引
7
次
|
|
|
|
2.
薛春纪. 滇西兰坪盆地构造体制和成矿背景分析.
矿床地质,2002,21(1):36-44
|
CSCD被引
70
次
|
|
|
|
3.
朱创业. 兰坪-思茅中生代盆地性质及构造演化.
成都理工学院学报,1997,24(4):23-30
|
CSCD被引
33
次
|
|
|
|
4.
阙梅英. 兰坪-思茅盆地铜矿床[M].
兰坪-思茅盆地铜矿床,1998:1-36
|
CSCD被引
20
次
|
|
|
|
5.
李任伟. 沉积地球化学[A].
地球化学:历史、现状和发展趋势,1996:86-96
|
CSCD被引
1
次
|
|
|
|
6.
Rollinson H R. evaluation.
Using geochemical data: evaluation, presentation, interpretation,1993:1-352
|
CSCD被引
112
次
|
|
|
|
7.
陈刚. 中生代鄂尔多斯盆地陆源碎屑成分及其构造属性.
沉积学报,1999,17(3):409-413
|
CSCD被引
28
次
|
|
|
|
8.
邵磊. 从砂岩成分探讨吐哈盆构造演化.
地质论评,2001,47(1):19-26
|
CSCD被引
13
次
|
|
|
|
9.
Bhatia M R. Plate tectonics and geochemical composition of sandstones[J].
Journal of Geology,1983,91:611-627
|
CSCD被引
465
次
|
|
|
|
10.
Bhatia M R. Provenance and tectonic control[J].
Sedimentary Geology,1985,45:97-113
|
CSCD被引
373
次
|
|
|
|
11.
Bhatia M R. Trace elemnt characteristics of graywackes and tectonic setting discrimination of sedimentary basin[J].
Contributions to Mineralogy and Petrology,1986,92:181-193
|
CSCD被引
687
次
|
|
|
|
12.
Roser B P. Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio[J].
Journal of Geology,1986,94:635-650
|
CSCD被引
371
次
|
|
|
|
13.
Roser B P. Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major element data[J].
Chemical Geology,1988,67:119-139
|
CSCD被引
325
次
|
|
|
|
14.
方维萱. 云南哀牢山地区构造岩石地层单元及其构造演化.
大地构造与成矿学,2002,26(1):28-36
|
CSCD被引
43
次
|
|
|
|
15.
冯庆来. 滇西北金沙江带被动陆缘地层层序和构造演化.
地球科学-中国地质大学学报,1999,24(6):553-557
|
CSCD被引
14
次
|
|
|
|
16.
何科昭. 滇西造山带的形成与演化.
地质论评,1996,42(2):97-106
|
CSCD被引
25
次
|
|
|
|
17.
Taylor S R. its composition and evolution[M].
The continental crust: its composition and evolution,1985:311
|
CSCD被引
6
次
|
|
|
|
18.
Mclennan S M. influence of provenance and sedimentary processes[J].
Reviews in Mineralogy,1989,21:169-200
|
CSCD被引
389
次
|
|
|
|
19.
Mclennan S M. geochemical and Nd-Pb isotopic evidence from metasedimentary rocks.
Geochimica et Cosmochimica Acta,1995,59:1153-1177
|
CSCD被引
98
次
|
|
|
|
20.
邵磊. 从砂岩地球化学探讨盆地构造背景.
科学通报,1998,43(9):985-987
|
CSCD被引
18
次
|
|
|
|
|