Detail publikačního výsledku

Lamprophyres, Lamproites and Related Rocks: Tracers to Supercontinent Cycles and Metallogenesis

KRMÍČEK, L.; CHALAPATHI RAO, N.V.

Originální název

Lamprophyres, Lamproites and Related Rocks: Tracers to Supercontinent Cycles and Metallogenesis

Anglický název

Lamprophyres, Lamproites and Related Rocks: Tracers to Supercontinent Cycles and Metallogenesis

Druh

Kniha (jiná než odborná)

Originální abstrakt

Paleoproterozoic to Cenozoic lamprophyres, lamproites and related rock types (e.g., orangeites, kimberlites) are volatile-rich mafic magmatic rocks with a unique potential for the investigation of processes affecting mantle reservoirs. They originated from primary mantle-derived melts that intruded both cratons and offcraton regions, which were parts of former supercontinents – Columbia, Rodinia and Gondwana–Pangea. Well-known for hosting economic minerals and elements such as diamonds, base metals, gold and platinum- group elements, they are also significant for our understanding of deep-mantle processes, such as mantle metasomatism and mantle plume–lithosphere interactions, as well as large-scale geodynamic processes, such as subduction-related tectonics, and supercontinent amalgamation and break-up. This book aims to provide a timely overview of the state-of-the-art and recent advances as achieved by various research groups around the world. Mineralogical, geochemical, geochronological and isotope analyses are used to decipher the complex petrogenesis and metallogenesis of these extraordinary rocks, and unravel a complete history of tectonic events related to individual supercontinent cycles.

Anglický abstrakt

Paleoproterozoic to Cenozoic lamprophyres, lamproites and related rock types (e.g., orangeites, kimberlites) are volatile-rich mafic magmatic rocks with a unique potential for the investigation of processes affecting mantle reservoirs. They originated from primary mantle-derived melts that intruded both cratons and offcraton regions, which were parts of former supercontinents – Columbia, Rodinia and Gondwana–Pangea. Well-known for hosting economic minerals and elements such as diamonds, base metals, gold and platinum- group elements, they are also significant for our understanding of deep-mantle processes, such as mantle metasomatism and mantle plume–lithosphere interactions, as well as large-scale geodynamic processes, such as subduction-related tectonics, and supercontinent amalgamation and break-up. This book aims to provide a timely overview of the state-of-the-art and recent advances as achieved by various research groups around the world. Mineralogical, geochemical, geochronological and isotope analyses are used to decipher the complex petrogenesis and metallogenesis of these extraordinary rocks, and unravel a complete history of tectonic events related to individual supercontinent cycles.

Klíčová slova

lamprophyres; lamproites; orangeites; kimberlites; supercontinents

Klíčová slova v angličtině

lamprophyres; lamproites; orangeites; kimberlites; supercontinents

Autoři

KRMÍČEK, L.; CHALAPATHI RAO, N.V.

Rok RIV

2022

Vydáno

09.02.2022

Nakladatel

Geological Society of London

Místo

Bath

ISBN

978-1-78620-543-8

Kniha

Lamprophyres, Lamproites and Related Rocks: Tracers to Supercontinent Cycles and Metallogenesis

Edice

513

Strany počet

489

URL

BibTex

@book{BUT176741,
  author="Lukáš {Krmíček} and N.V. {Chalapathi Rao}",
  title="Lamprophyres, Lamproites and Related Rocks: Tracers to Supercontinent Cycles and Metallogenesis",
  year="2022",
  publisher="Geological Society of London",
  address="Bath",
  series="513",
  edition="1",
  pages="489",
  doi="10.1144/SP513",
  isbn="978-1-78620-543-8",
  url="https://www.geolsoc.org.uk/SP513"
}