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Title:	Death and Transfiguration of a Triple Junction in the South Atlantic
Source:	Science [0036-8075] Ligi, M yr:1997

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description	15.	Vermeesch, Pieter, P. "Multimethod detrital thermochronology of the Great Valley Group near New Idria, California." Geological Society of America bulletin 118.1-2 (2006): 210-218.
description	16.	Smith, Wenlu K. "The recent history of the Galapagos triple junction preserved on the Pacific plate." Earth and planetary science letters 371-372.C (2013): 6-15.
description	17.	Hayman, Toshiya W. "Structural evolution of an inner accretionary wedge and forearc basin initiation, Nankai margin, Japan." Earth and planetary science letters 353-354 (2012): 163-172.
description	18.	Brandmeier, M. "New challenges for tafoni research. A new approach to understand processes and weathering rates." Earth surface processes and landforms 36.6 (2010): 839-852.
description	19.	Lonsdale, P. "The RRR triple junction at the southern end of the Pacific-Cocos East Pacific Rise." Earth and planetary science letters 109.1-2 (1992): 73-85.
description	20.	Georgen, Jennifer E. "Effects of ridge geometry on mantle dynamics in an oceanic triple junction region; implications for the Azores Plateau." Earth and planetary science letters 298.1-2 (2010): 23-34.