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Petrogenesis and geochronology of Cretaceous adakitic, I- and A-type granitoids in the NE Yangtze block: Constraints on the eastern subsurface boundary between the North and South China blocks: Reply
被引:1
|作者:
Su, Yuping
[1
,2
,3
]
Zheng, Jianping
[1
,2
,3
]
Griffin, William L.
[2
,3
]
Zhao, Junhong
[1
]
O'Reilly, Suzanne Y.
[2
,3
]
Tang, Huayun
[1
]
Ping, Xianquan
[1
]
Xiong, Qing
[1
,2
,3
]
机构:
[1] China Univ Geosci, Fac Earth Sci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
[2] Macquarie Univ, ARC Ctr Excellence Core Crust Fluid Syst CCFS, N Ryde, NSW 2109, Australia
[3] Macquarie Univ, Dept Earth & Planetary Sci, GEMOC, N Ryde, NSW 2109, Australia
来源:
基金:
澳大利亚研究理事会;
关键词:
Adakites;
Subsurface boundary;
The Yangtze block;
Precambrian basement;
U-PB GEOCHRONOLOGY;
PROVIDE GEOCHEMICAL FINGERPRINTS;
CRUSTAL-DETACHMENT MODEL;
LU FAULT ZONE;
ISOTOPIC COMPOSITIONS;
GRANULITE XENOLITHS;
CENOZOIC BASALTS;
ANHUI PROVINCE;
IGNEOUS ROCKS;
TANLU FAULT;
D O I:
10.1016/j.lithos.2014.02.024
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
We thank Zeng and Yan (2014) for their interest in our recent paper "Petrogenesis and geochronology of Cretaceous adakitic, I- and A-type granitoids in the NE Yangtze block: Constraints on the eastern subsurface boundary between the North and South China blocks". However, Zeng and Yan (2014) have misinterpreted some available data and literature regarding the basement in the Yangtze block. After carefully rechecking available isotopic data for the Precambrian basement and providing additional arguments, we show that their arguments are not correct, and confirm that our viewpoint on the source of the Chuzhou adakitic rocks and eastern subsurface boundary between the North and South China blocks remains valid. (C) 2014 Elsevier B.V. All rights reserved.
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页码:380 / 383
页数:4
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