Pb-, Sr- and Nd-isotopic systematics and chemical characteristics of Cenozoic basalts, eastern China

Extension-related origin of magmas from a garnet-bearing source in the Los Tuxtlas volcanic field, Mexico

“…The rifts represented in this database are: Rio Grande, USA (Johnson and Lipman 1988;Duncker et al 1991;Gibson et al 1992;McMillan et al 2000); Abu Gabra (Davidson and Wilson 1989); East Africa (Aoki et al 1985;De Mulder et al 1986;Auchapt et al 1987;Class et al 1994); Ethiopia (Barberi et al 1975;Hart et al 1989;Trua et al 1999;Deniel et al 1994;Barrat et al 2003); Gregory (Macdonald et al 1995); and Kenya (Bell and Peterson 1991;Le Roex et al 2001;Macdonald et al 2001). Similarly, the extension-related or intraplate-type volcanic fields are: Basin and Range, USA (Singer and Kudo 1986;Lum et al 1989;Moyer and Esperanc¸a 1989;Perry et al 1990;Fitton et al 1991); Hurricane volcanic field, Utah (Smith et al 1999); Western USA (Kempton et al 1991); San Quintı´n volcanic field, Baja California, Mexico (Rogers et al 1985;Saunders et al 1987;Storey et al 1989;Luhr et al 1995); Massif Central, France (Chauvel and Jahn 1984); Saudi Arabia (Camp et al 1991); Taiwan strait (Chung et al 1994); northwestern Taiwan (Chung et al 1995); Eastern China (Peng et al 1986;Zhi et al 1990;Basu et al 1991;Fan and Hooper 1991;…”

Early Cretaceous gabbroic complex from Yinan, Shandong Province: petrogenesis and mantle domains beneath the North China Craton

“…6g, h). Because Ni is compatible in Ol and Cr is compatible in Cpx and (Peng et al 1986;Basu et al 1991;Song et al 1990;Liu et al 1995) and Mesozoic magmas from western Shandong (Guo et al , 2003 and from Fangcheng are given for comparison. The field for the Dabie mafic and ultramafic intrusions is after Li et al (1998) and Jahn et al (1999).…”

“…6d). and Cenozoic basalts (Peng et al 1986;Basu et al 1991;Song et al 1990) are shown for comparison. Field of lower crust granulites is after Zhou et al (2002).…”

Continental dynamics of Eastern China: Insights from tectonic history and receiver function analysis

“…Widespread intraplate magmatism occurred during the Mesozoic in the NCC which has been attributed to plumes associated with the re-activation/delamination of the NCC (Flower et al, 1998;Peng et al, 1986;Zhao et al, 2004b;Menzies et al, 2007). Different models also consider the asthenosphere upwelling and the upwelling mantle plume resulting in the lithospheric thinning of the NCC (Menzies and Xu, 1998;Deng et al, 2004;.…”