Tectonothermal evolution of the continental crust beneath the Yakutian diamondiferous province (Siberian craton): U-Pb and Hf isotopic evidence on zircons from crustal xenoliths of kimberlite pipes
详细信息 查看全文
- 作者：V.S. Shatskya ; b ; c ; ; V.G. Malkovetsb ; d ; e ; E.A. Belousovae ; I.G. Tretiakovab ; e ; W.L. Griffine ; A.L. Ragozinb ; A.A. Gibsherb ; d ; S.Y. O&rsquo ; Reillye
- 关键词：Yakutian kimberlite province ; Crustal xenoliths ; Zircon ; U&ndash ; Pb dating ; Lu&ndash ; Hf isotope system ; Continental crust evolution
- 刊名：Precambrian Research
- 出版年：2016
- 出版时间：September 2016
- 年：2016
- 卷：282
- 期：Complete
- 页码：1-20
- 全文大小：1572 K
文摘
- •
The Paleoarchean crust of the Markha terrain was significantly reworked.
- •
Crustal xenoliths record the same events that occurred in the adjacent Daldyn and Magan terranes.
- •
It is not correct to distinguish Markha as a separate terrane.