@article {Moeller2014,
	title = {{Crustal thinning in the northern Tyrrhenian Rift: Insights from multichannel and wide-angle seismic data across the basin}},
	volume = {119},
	number = {3},
	year = {2014},
	pages = {1655{\textendash}1677},
	url = {http://apps.isiknowledge.com/full\_record.do?product=UA\&search\_mode=GeneralSearch\&qid=5\&SID=S1AN85ZGXvSBJ7DKZfo\&page=1\&doc=3},
	author = {Moeller, S. and Grevemeyer, I. and Ranero, C. R.}
}
@article {Dannowski2011,
	title = {{Crustal structure of the propagating TAMMAR ridge segment on the Mid-Atlantic Ridge, 21.5{\textdegree}N}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {12},
	number = {7},
	year = {2011},
	month = {jul},
	pages = {n/a{\textendash}n/a},
	abstract = {Active ridge propagation frequently occurs along spreading ridges and profoundly affects ridge crest segmentation over time. The mechanisms controlling ridge propagation, however, are poorly understood. At the slow spreading Mid-Atlantic Ridge at 21.5{\textdegree}N a seismic refraction and wide-angle reflection profile surveyed the crustal structure along a segment controlled by rapid ridge propagation. Tomographic traveltime inversion of seismic data suggests that the crustal structure along the ridge axis is controlled by melt supply; thus, crust is thickest, 8 km, at the domed segment center and decreases in thickness toward both segment ends. However, thicker crust is formed in the direction of ridge propagation, suggesting that melt is preferentially transferred toward the propagating ridge tip. Further, while seismic layer 2 remains constant along axis, seismic layer 3 shows profound changes in thickness, governing variations in total crustal thickness. This feature supports mantle upwelling at the segment center. Thus, fluid basaltic melt is redistributed easily laterally, while more viscose gabbroic melt tends to crystallize and accrete nearer to the locus of melt supply. The onset of propagation seems to have coincided with the formation of thicker crust, suggesting that propagation initiation might be due to changes in the melt supply. After a rapid initiation a continuous process of propagation was established. The propagation rate seems to be controlled by the amount of magma that reaches the segment ends. The strength of upwelling may govern the evolution of ridge segments and hence ultimately controls the propagation length. Copyright 2011 by the American Geophysical Union.},
	keywords = {Crustal structure, mid-ocean ridges, ridge propagation, seismic traveltime tomography},
	issn = {15252027},
	doi = {10.1029/2011GC003534},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-79960696393\&partnerID=tZOtx3y1},
	author = {Dannowski, A. and Grevemeyer, I. and Phipps Morgan, J. and Ranero, C. R. and Maia, M. and Klein, G.}
}
@inbook {RaneroC.R.;vonHueneR.;WeinrebeW.andBarckhausen2007,
	title = {{Convergent margin tectonics of Middle America: A marine perspective}},
	booktitle = {Central America, Geology, Hazards and Resources},
	year = {2007},
	pages = {239{\textendash}265},
	keywords = {A. A. Balkema Publisher)., Ed. G. Alvarado and J. Bunschu},
	url = {http://sfx.bibliotecas.csic.es/sfx\_local?url\_ver=Z39.88-2004\&rft\_val\_fmt=info\%3Aofi\%2Ffmt\%3Akev\%3Amtx\%3Abook\&rft.genre=bookitem\&rft.btitle=Central America\%3A Geology\%2C Resources and Hazards\&rft.spage=239\&rft.epage=265\&rft.date=2007\&rft.aulast=Ranero\&},
	author = {Ranero, C. R. and von Huene, R. and Weinrebe, W. and Barckhausen, U.}
}
@article {Booth-Rea2007,
	title = {{Crustal types and Tertiary tectonic evolution of the Albor{\'a}n sea, western Mediterranean}},
	journal = {Geochemistry, Geophysics, Geosystems},
	volume = {8},
	number = {10},
	year = {2007},
	pages = {n/a{\textendash}n/a},
	abstract = {Multichannel seismic reflection images across the transition between the east Albor{\'a}n and the Algero-Balearic basins show how crustal thickness decreases from about 5 s two-way traveltime (TWTT, \~{}15 km thick) in the west (east Albor{\'a}n basin) to \~{}2 s TWTT typical of oceanic crust (\~{}6 km thick) in the east (Algero-Balearic basin). We have differentiated three different crustal domains in this transition, mainly on the basis of crustal thickness and seismic signature. Boundaries between the three crustal domains are transitional and lack evidence for major faults. Tilted blocks related to extension are very scarce and all sampled basement outcrops are volcanic, suggesting a strong relationship between magmatism and crustal structure. Stratigraphic correlation of lithoseismic units with sedimentary units of southeastern Betic basins indicates that sediments onlap igneous basement approximately at 12 Ma in the eastern area and at 8 Ma in the western area. Linking seismic crustal structure with magmatic geochemical evidence suggests that the three differentiated crustal domains may represent, from west to east, thin continental crust modified by arc magmatism, magmatic-arc crust, and oceanic crust. Middle to late Miocene arc and oceanic crust formation in the east Albor{\'a}n and Algero-Balearic basins, respectively, occurred during westward migration of the Gibraltar accretionary wedge and shortening in the Betic-Rif foreland basins. Arc magmatism and associated backarc oceanic crust formation were related to early to middle Miocene subduction and rollback of the Flysch Trough oceanic basement. Subduction of this narrow slab beneath the Albor{\'a}n basin was coeval with collision of the Albor{\'a}n domain with the Iberian and African passive margins and subsequent subcontinental- lithosphere edge delamination along the Betic-Rif margins. Copyright 2007 by the American Geophysical Union.},
	keywords = {Albor{\'a}n basin, Algero-Balearic basin, Crustal structure, Magmatic arc, Reflection seismics, Western Mediterranean},
	issn = {15252027},
	doi = {10.1029/2007GC001639},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-54349126940\&partnerID=tZOtx3y1},
	author = {Booth-Rea, G. and Ranero, C. R. and Mart{\'\i}nez-Mart{\'\i}nez, J. M. and Grevemeyer, I.}
}
