山东东部早白垩世青山期穿地壳岩浆系统与热隆滑脱成盆

周瑶琪; 周腾飞; 马昌前; 张振凯; 董诗绘; 辜洋建; 尹兴城; 李曼洁; 梁文栋

doi:10.3799/dqkx.2018.998

Volume 43 Issue 10

Oct. 2018

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Article Navigation > Earth Science > 2018 > 43(10): 3373-3390

Zhou Yaoqi, Zhou Tengfei, Ma Changqian, Zhang Zhenkai, Dong Shihui, Gu Yangjian, Yin Xingcheng, Li Manjie, Liang Wendong, 2018. Transcrustal Magmatic System of Early Cretaceous (Qingshan Stage) in Eastern Shandong and the Basin Formation Related to 'Thermal Upwelling-Detachment'. Earth Science, 43(10): 3373-3390. doi: 10.3799/dqkx.2018.998

Citation:

Zhou Yaoqi, Zhou Tengfei, Ma Changqian, Zhang Zhenkai, Dong Shihui, Gu Yangjian, Yin Xingcheng, Li Manjie, Liang Wendong, 2018. Transcrustal Magmatic System of Early Cretaceous (Qingshan Stage) in Eastern Shandong and the Basin Formation Related to "Thermal Upwelling-Detachment". Earth Science, 43(10): 3373-3390. doi: 10.3799/dqkx.2018.998

Citation:

Zhou Yaoqi, Zhou Tengfei, Ma Changqian, Zhang Zhenkai, Dong Shihui, Gu Yangjian, Yin Xingcheng, Li Manjie, Liang Wendong, 2018. Transcrustal Magmatic System of Early Cretaceous (Qingshan Stage) in Eastern Shandong and the Basin Formation Related to "Thermal Upwelling-Detachment". Earth Science, 43(10): 3373-3390. doi: 10.3799/dqkx.2018.998

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Transcrustal Magmatic System of Early Cretaceous (Qingshan Stage) in Eastern Shandong and the Basin Formation Related to "Thermal Upwelling-Detachment"

doi: 10.3799/dqkx.2018.998

1.
School of Geosciences, China University of Petroleum, Qingdao 266580, China
2.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
3.
School of Earth Science, China University of Geosciences, Wuhan 430074, China
4.
Shanxi Institute of Geological Survey, Shanxi Center of Geological Survey, Xi'an 710068, China
5.
Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milano 20126, Italy

Received Date: 2018-05-04
Publish Date: 2018-10-20

Abstract

Abstract

A new conception of magmatic system-transcrustal magmatic system(TMS) has been raised recently. This paper focuses on the TMS of Early Cretaceous (Qingshan stage) in Eastern Shandong. Based on the geological field work and the research results of igneous chronology, distribution of fault system, tectonics and geochemistry, we discuss the temporal and spatial evolution and distribution characteristics of different volcanic magmatism. Firstly, the TMS varies from silicic magmatic emplacement to basic magmatic intrusion and then to medium magmatic eruption. Secondly, the TMS owes different behaviors at different depths of crust:from deep to shallow, TMS behaves in the sequence of Batholith/Stock-Intrusions/Dike-volcanic edifice. Thirdly, the silicic batholith/stock is mainly distributed in old uplift zone, while the volcanic edifice is mainly distributed along the deep fault. The development of TMS indicates the structure characteristics of lithosphere in Qingshan stage:The nearly E-W distribution of the stock itself shows the fault system in upper crust is nearly E-W when the magma flows upward. While the distribution of all the batholiths/stocks is in the direction of NE-SW, indicating that the deep fault system is in the direction of NE-SW, which controls the regional tectonic evolution. In Early Cretaceous, the shallow fault system developed in Laiyang stage provided the channel for the TMS developed in Qingshan stage. In the development period of TMS, there was strong "thermal-upwelling, stretching and detachment" effect, which resulted in the basin framework in Qingshan stage. The calculated rate of granite uplift related to thermal-upwelling is slightly faster than 2.47-3.7 mm/a. The intense "thermal-upwelling, stretching and detachment" effect is the main dynamic mechanism of basin formation in Qingshan stage.
- eastern Shandong,
- Cretaceous,
- transcrustal magmatic system,
- basin dynamics,
- petroleum geology

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References(92)

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Transcrustal Magmatic System of Early Cretaceous (Qingshan Stage) in Eastern Shandong and the Basin Formation Related to "Thermal Upwelling-Detachment"

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