Titlebook: Dyke Swarms of the World: A Modern Perspective; Rajesh K. Srivastava,Richard E. Ernst,Peng Peng Book 2019 Springer Nature Singapore Pte Lt

overreach

奴才

Andreas Flitner,Christian Petry,Ingo Richters with synchronous lithosphere extension during the two time periods. The Avanavero (1.79 Ga) LIP event mostly consists of mafic dykes and sills which are intrusive into the Roraima platform cover, in the Guiana Shield. They show tholeiitic chemistry and similarities with E-MORB and subcontinental l

Panther

apiary

Jürgen Oßenbrügge,Susanne Heeg,Britta Klagge sills in the Taoudeni basin. The last ones are related to the Central Atlantic Magmatic Province (CAMP) event. The Hounde swarm is oblique to the dominant radiating CAMP swarm and may be linked with the similar-trending elongate Kakoulima intrusion in Guinea. In addition, the N150° Käyser swarm (Am

低三下四之人

Jürgen Oßenbrügge,Susanne Heeg,Britta Klaggesia, and is intended to provide basic preparation for more in-depth studies in the future. In Enhanced Thematic Mapper Plus (bands 7, 4, and 2) images, major mafic dykes (greater than 5 m wide) displayed as dark-colored linear objects against their host rocks, and can be distinguished and plotted on

FIN

Wachsende Stadt — Nachhaltige Stadtn shield and their matches with coeval LIPs on other crustal blocks suggest connections of the Indian shield within known supercontinents, such as Kenorland/Superia (~2.75–2.07 Ga), Columbia/Nuna (1.90–1.38 Ga), and Rodinia (1.20–0.72 Ga). However, further detailed U–Pb geochronology and associated

cacophony

ectropion

吞下

轨道

The Precambrian Mafic Magmatic Record, Including Large Igneous Provinces of the Kalahari Craton and