The Origin of Mesoarchaean Granitic Rocks from Anshan-Benxi Area: Constraints of Geochemistry and Nd Isotope;辽宁鞍山-本溪地区中太古代花岗质岩石的成因-地球化学及Nd同位素制约

Yanshi Xuebao/Acta Petrologica Sinica

Volumn 14, Issue 3, 1998, Pages 278-288

  Wan, Yusheng ^a   Liu, Dunyi ^a   Wu, Jiashan ^a   Zhang, Zongqing ^a   Song, Biao ^a  

^a INSTITUTE OF GEOLOGY   (China)

Author keywords

Anshan Benxi area; Geochemistry; Granitic rocks; Mesoarchaean; Sm Nd isotope

Indexed keywords

EID: 85168645174     PISSN: 10000569     EISSN: 20958927     Source Type: Journal    
DOI: None     Document Type: Article

References (6)

1. Bea K. 1996. Residence of REEi Y, Th and U in granites and crustal protoliths (implications for the chemistry of crust si melts. Journal of Petrology, 37 (3). 521—552
2. Liu D Y, Nutman A P, Compston W, Wu J S and Shen Q H. 1992. Remnants of >3800 Ma crust in the Chinese part of the Sino-Korean craton, Geology, 20: 339 — 342
3. : Archean crustal evolution, Elsevier. Amsterdam., 205 — 259
4. Song B, Nutman A P, Liu D Y and Wu J S. 1996. 3800 to 25O0 Ma crust in the Anshan area of Liaoning Province, northeastern China. Precambrian Research, 78: 79~94
5. Sun M, Armstrong R L, Lambert R J, Jiang C C and Wu J H. 1993. Petrochemistry and Sr, Pb and Nd isotopic geochemistry of the Paleoproterozoic Kuandian complex, the eastern Liaoning Province, China. Precambian Research. 62i 171 — 190
6. : their geochemistry, metomorphism and petro genes is, Precambrain Research, 46: 195—216