Part 3 : Fault Zone Structure, Composition, and Physical Properties Drilling the Seismogenic Zone of an Erosional Convergent Margin: IODP Costa Rica Seismogenesis Project CRISP by César R. Ranero, Paola Vannucchi, Rola

First Page		Document Content
Date: 2014-12-05 03:20:38 Accretionary wedge Megathrust earthquake Integrated Ocean Drilling Program Earthquake Scientific drilling Interplate earthquake Forearc Nankai Trough Geology Plate tectonics Subduction		Part 3 : Fault Zone Structure, Composition, and Physical Properties Drilling the Seismogenic Zone of an Erosional Convergent Margin: IODP Costa Rica Seismogenesis Project CRISP by César R. Ranero, Paola Vannucchi, Rola Add to Reading List Source URL: www.sci-dril.net Download Document from Source Website File Size: 1,94 MB Share Document on Facebook

	Contents 1 Geofactors & ecozones 6 5 Ways into the future Plate tectonics – Endogenous forces shaping the Earth 8 DocID: 1uDhc - View Document
	Exploring the Earth from Mars David T. Sandwell Scripps Institution of Oceanography December, To be published in: Plate tectonics, Stories of Discovery, editors, N. Oreskes and H. LeGrand, Columb DocID: 1umzZ - View Document
	Oceanography 101 First & Last Name_____________________ Laboratory Exercise #2: Sea-Floor Spreading and Plate Tectonics DocID: 1sJAA - View Document
	Worksheet: Plate Tectonics name: *Use sentences. (starts on page 248 of your text) 1. First read pagesLook at the map A on page 251. About how many million years ago did DocID: 1sCtJ - View Document
	Worksheet: Plate Tectonics name: *Use sentences. (starts on page 194 of the honors text) 1. Look at the map atop page 195. About how many million years ago did the Earth look like this? DocID: 1souO - View Document