Overlapping A-type and S-type characters in late- to post-tectonic granites – petro-tectonic evolution of late Mesoproterozoic Andhra Konda granite, Nellore Schist Belt, southern India

[1] Abdel-Rahman AM(1994)Nature of biotites from alkaline, calc-alkaline and peraluminous magma J. Petrol. 35 525-541

[2] Bickford ME(2015)Mesoproterozoic-trans-Laurentian magmatism: A synthesis of continent-wide age distributions, new SIMSU–Pb ages, zircon saturation temperatures, and Hf and Nd isotopic compositions Precamb. Res. 265 286-312

[3] van Schmus WR(2007)A-type granites and related rocks: Evolution of a concept, problems and prospects Lithos 97 1-29

[4] Karlstorm KE(1981)The mineralogy of peraluminous granites: A review Can. Mineral. 19 3-17

[5] Mueller PA(1982)Nature and origin of A-type granites with particular reference to south-eastern Australia Contrib. Mineral. Petrol. 80 189-200

[6] Kamenov GD(2019)Repeated S–I–A-type granite trilogy in the Lachlan Orogen and geochemical contrasts with A-type granites in Nigeria: Implications for petrogenesis and tectonic discrimination Geol. Soc. Spec. Publ. 491 53-76

[7] Bonin B(1993)Chemical composition and evolution of the upper continental crust: Contrasting results from surface samples and shales Chem. Geol. 104 1-37

[8] Clarke DB(2012)IGCP Project 510 ‘A-type Granites and Related Rocks through Time’: Project vita, results, and contribution to granite research Lithos 151 1-16

[9] Collins WJ(2016)Evidences of inclined transpression at the contact between Vinjamuru group and Udayagiri group of Nellore Schist Belt, Andhra Pradesh, India J. Earth Syst. Sci. 125 1007-1020

[10] Beams SD(2007)Petrology and geochemistry of Paleoproterozoic A-type granite at Kanigiri in the Nellore–Khammam schist belt, Andhra Pradesh, India J. Asian Earth Sci. 30 1-19

[1] Abdel-Rahman AM(1994)Nature of biotites from alkaline, calc-alkaline and peraluminous magma J. Petrol. 35 525-541

[2] Bickford ME(2015)Mesoproterozoic-trans-Laurentian magmatism: A synthesis of continent-wide age distributions, new SIMSU–Pb ages, zircon saturation temperatures, and Hf and Nd isotopic compositions Precamb. Res. 265 286-312

[3] van Schmus WR(2007)A-type granites and related rocks: Evolution of a concept, problems and prospects Lithos 97 1-29

[4] Karlstorm KE(1981)The mineralogy of peraluminous granites: A review Can. Mineral. 19 3-17

[5] Mueller PA(1982)Nature and origin of A-type granites with particular reference to south-eastern Australia Contrib. Mineral. Petrol. 80 189-200

[6] Kamenov GD(2019)Repeated S–I–A-type granite trilogy in the Lachlan Orogen and geochemical contrasts with A-type granites in Nigeria: Implications for petrogenesis and tectonic discrimination Geol. Soc. Spec. Publ. 491 53-76

[7] Bonin B(1993)Chemical composition and evolution of the upper continental crust: Contrasting results from surface samples and shales Chem. Geol. 104 1-37

[8] Clarke DB(2012)IGCP Project 510 ‘A-type Granites and Related Rocks through Time’: Project vita, results, and contribution to granite research Lithos 151 1-16

[9] Collins WJ(2016)Evidences of inclined transpression at the contact between Vinjamuru group and Udayagiri group of Nellore Schist Belt, Andhra Pradesh, India J. Earth Syst. Sci. 125 1007-1020

[10] Beams SD(2007)Petrology and geochemistry of Paleoproterozoic A-type granite at Kanigiri in the Nellore–Khammam schist belt, Andhra Pradesh, India J. Asian Earth Sci. 30 1-19