中国东北及邻区白垩纪岩浆活动与古太平洋板块俯冲的关系
Cretaceous Magmatism in NE China and Adjacent Areas and Its Relationship with the Paleo-Pacific Plate Subduction
查看参考文献81篇
文摘
|
本文简要综述了古太平洋构造演化历史和中国东北及邻区构造单元,总结了中国东北及邻区白垩纪岩浆活动的时空分布规律及岩石组合特征,认为中国东北额尔古纳-兴安-松辽-佳木斯地块145 ~ 88 Ma岩浆活动显著,从西向东由老变新,特征岩石组合为软流圈地幔来源玄武质岩石,以及Ⅰ型和A型花岗岩类; 88~ 65 Ma岩浆活动较弱,仅少量OIB型玄武岩。完达山-锡霍特-阿林-延边地区白垩纪岩浆活动也具有从西向东由老变新的规律,特征岩石组合为高镁安山岩、埃达克岩、I型及S型花岗岩等中酸性岩石。上述岩浆活动分别形成于弧后(板内)及大陆弧。中国东北早白垩世大陆弧具有弧后伸展,与年老大洋岩石圈的俯冲有关,是现代地球上少见的俯冲类型; 晚白垩世中晚期,弧后发生构造挤压,与智利型大陆边缘相似。 |
其他语种文摘
|
This paper briefly reviewed the tectonic evolution history of the Paleo-Pacific Plate and tectonic regimes of NE China and adjacent areas. It also summarized the spatial and temporal association and petrogenesis of Cretaceous igneous rocks,proposing its relationship with Paleo-Pacific Plate subduction. The Erguna,Xing'an,Songliao,and Jiamusi blocks of NE China have significant igneous activities in 145-88 Ma,characterized by a spatial and temporal eastward migration and an association of I-and A-type granites and asthenosphere-derived basaltic rocks,with minor OIB-type basalts after~ 88 Ma. The Cretaceous magmatism in the Wandashan-Sikhote-Alin and Yanbian area is also characterized by eastward migration but an association of intermediate to acidic rocks including high-Mg andesites,adakites,and I-and S-type granites. Cretaceous magmatism in Erguna-Xing'an-Songliao-Jiangmusi and Wandashan-Sikhote-Alin-Yanbian areas was thought to be formed in back-arc(intra-plate) and continental arc settings,respectively,and was controlled by roll-back of the Paleo- Pacific Plate. The Early Cretaceous continental arc accompanied with back-arc extension was most likely to result from subduction of old oceanic lithosphere,which rarely occurred in the modern earth. The Late Cretaceous continental arc at NE China,characterized by back-arc compression,was similar to the present Chilean continental margin. |
来源
|
矿物岩石地球化学通报
,2016,35(6):1090-1097 【核心库】
|
DOI
|
10.3969/j.issn.l007-2802.2016.06.003
|
关键词
|
活动大陆边缘
;
古太平洋
;
白垩纪
;
俯冲后撤
|
地址
|
中国科学院广州地球化学研究所, 同位素地球化学国家重点实验室, 广州, 510640
|
语种
|
中文 |
ISSN
|
1007-2802 |
学科
|
地质学 |
基金
|
国家973计划
|
文献收藏号
|
CSCD:5901615
|
参考文献 共
81
共5页
|
1.
Cawood P A. Linking collisional and accretionary orogens during Rodinia assembly and breakup: Implications for models of supercontinent cycles.
Earth and Planetary Science Letters,2016,449:118-126
|
被引
36
次
|
|
|
|
2.
Cui F H. Detrital zircon ages of the Jiageda and Woduhe formations: Constrains on the tectonic attribute of the Xing' an terrane in the central Great Xing' an Range,NE China.
Journal of Asian Earth Sciences,2015,113:427-442
|
被引
15
次
|
|
|
|
3.
Defant M J. Derivation of some modern arc magmas by melting of young subducted lithosphere.
Nature,1990,347(6294):662-665
|
被引
1277
次
|
|
|
|
4.
Fan W M. Late Mesozoic calc-alkaline volcanism of post-orogenic extension in the northern Da Hinggan Mountains,northeastern China.
Journal of Volcanology and Geothermal Research,2003,121(1/2):115-135
|
被引
161
次
|
|
|
|
5.
Feng Z Q. Tectonostratigraphic units and stratigraphic sequences of the nonmarine Songliao basin,northeast China.
Basin Research,2010,22(1):79-95
|
被引
94
次
|
|
|
|
6.
Feng Z Q. Timing and nature of the Xinlin-Xiguitu Ocean: Constraints from ophiolitic gabbros in the northern Great Xing'an Range,eastern Central Asian Orogenic Belt.
International Journal of Earth Sciences,2016,105(2):491-505
|
被引
21
次
|
|
|
|
7.
Frost C D. On Ferroan(A-type) Granitoids: Their compositional variability and modes of origin.
Journal of Petrology,2011,52(1):39-53
|
被引
83
次
|
|
|
|
8.
Ge W C. Tectonic implications of new zircon U-Pb ages for the Xinghuadukou Complex,Erguna Massif,northern Great Xing'an Range,NE China.
Journal of Asian Earth Sciences,2015,106:169-185
|
被引
23
次
|
|
|
|
9.
Grebennikov A V. Cretaceous and Paleogene granitoid suites of the Sikhote-Alin area (Far East Russia): Geochemistry and tectonic implications.
Lithos,2016,261:250-261
|
被引
5
次
|
|
|
|
10.
Jahn B M. Massive granitoid generation in Central Asia: Nd isotope evidence and implication for continental growth in the Phanerozoic.
Episodes,2000,23(2):82-92
|
被引
295
次
|
|
|
|
11.
Jahn B M. Emplacement ages,geochemical and Sr-Nd-Hf isotopic characterization of Mesozoic to early Cenozoic granitoids of the Sikhote-Alin Orogenic Belt,Russian Far East: Crustal growth and regional tectonic evolution.
Journal of Asian Earth Sciences,2015,111:872-918
|
被引
20
次
|
|
|
|
12.
Ji W Q. Chronology and geochemistry of volcanic rocks in the Cretaceous Suifenhe formation in eastern Heilongjiang,China.
Acta Geologica Sinica,2007,81(2):266-277
|
被引
12
次
|
|
|
|
13.
Kojima S. Mesozoic terrane accretion in northeast China,Sikhote-Alin and Japan regions.
Palaeogeography,Palaeoclimatology,Palaeoecology,1989,69:213-232
|
被引
31
次
|
|
|
|
14.
Kotov A B. Age of the amur group of the Bureya-Jiamusi Superterrane in the Central Asian fold belt: Sm-Nd isotope evidence.
Doklady Earth Sciences,2009,429(8):1245-1248
|
被引
3
次
|
|
|
|
15.
Kuang Y S. Petrogenetic evaluation of the Laohutai basalts from North China Craton: Melting of a two-component source during lithospheric thinning in the late Cretaceous-early Cenozoic.
Lithos,2012,154:68-82
|
被引
17
次
|
|
|
|
16.
Kuritani T. Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation.
Nature Geoscience,2011,4(10):713-716
|
被引
32
次
|
|
|
|
17.
Li W M. Newly discovered garnetbarroisite schists from the Heilongjiang Complex in the Jiamusi Massif, northeastern China.
Journal of Mineralogical and Petrological Sciences,2010,105(2):86-91
|
被引
8
次
|
|
|
|
18.
Muller R D. Longterm sea-level fluctuations driven by ocean basin dynamics.
Science,2008,319(5868):1357-1362
|
被引
56
次
|
|
|
|
19.
Maruyama S. Plume tectonics.
Geological Society of Japan,1994,100(1):24-49
|
被引
59
次
|
|
|
|
20.
Maruyama S. Superplume,supercontinent, and post-perovskite: Mantle dynamics and anti-plate tectonics on the Core-Mantle Boundary.
Gondwana Research,2007,11(1/2):7-37
|
被引
80
次
|
|
|
|
|