<html xmlns="http://www.w3.org/1999/xhtml" xmlns:v="urn:schemas-microsoft-com:vml" xmlns:o="urn:schemas-microsoft-com:office:office"><head><!--[if gte mso 9]><xml><o:OfficeDocumentSettings><o:AllowPNG/><o:PixelsPerInch>96</o:PixelsPerInch></o:OfficeDocumentSettings></xml><![endif]--></head><body><div class="yahoo-style-wrap" style="font-family:Helvetica Neue, Helvetica, Arial, sans-serif;font-size:13px;"><div dir="ltr" data-setdir="false"><div><h4 style="margin:0in;"><span style="font-size:15.0pt;font-family:sans-serif;color:#2E2E2E;">Journal of South American Earth Sciences - Promotional Access of Special Issues</span></h4> 
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<em><b><span style="font-family:sans-serif;"><a href="https://www.sciencedirect.com/journal/journal-of-south-american-earth-sciences" rel="nofollow" target="_blank">Journal of South American Earth Sciences</a></span></b></em><strong><span style="font-family:sans-serif;"> </span></strong>is
 pleased to announce that articles from below special issues are free to access on ScienceDirect until 20 Jan 2022.</p> 
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<p style="margin:0in;"><strong><span style="font-family:sans-serif;">“<a href="https://nam11.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.sciencedirect.com%2Fjournal%2Fjournal-of-south-american-earth-sciences%2Fspecial-issue%2F10Z2L86JV3F&data=04%7C01%7Cl.brett%40elsevier.com%7Caf812a6088ea4c5fa0c508d9828f3d37%7C9274ee3f94254109a27f9fb15c10675d%7C0%7C0%7C637684373998133731%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C1000&sdata=PiBVVEwTiWzGCjdXbsDhSpY80Px%2FtzVacZt14g4Dr1I%3D&reserved=0" rel="nofollow" target="_blank">Hazardous
 Faults in Latin America</a>”, guest edited by Carlos Costa, Laurence Audin</span></strong></p> 
<p style="margin-right:0in;margin-bottom:9.0pt;margin-left:0in;">
Subduction earthquakes are the most significant seismic threat for Latin
 America. However, destructive earthquakes related to shallow crustal 
sources have occurred onshore, where many important cities and critical 
facilities are settled nearby crustal fault
 sources. This Special Issue aims to provide to the Earth Sciences 
community and other potential users with case histories, recent 
advances, and present trends outcoming from the increasing information 
devoted to the geology of Seismogenic Sources.</p> 
<p style="margin:0in;"><strong><span style="font-family:sans-serif;">“<a href="https://nam11.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.sciencedirect.com%2Fjournal%2Fjournal-of-south-american-earth-sciences%2Fspecial-issue%2F10CV3PKFJGV&data=04%7C01%7Cl.brett%40elsevier.com%7Caf812a6088ea4c5fa0c508d9828f3d37%7C9274ee3f94254109a27f9fb15c10675d%7C0%7C0%7C637684373998133731%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C1000&sdata=O4aNpzmu3Tn9ujOPoHuL%2FqXtZzU9mmJPbc0NwRoz6YY%3D&reserved=0" rel="nofollow" target="_blank" class="enhancr_card_4930473850">Thermochronology
 in South America: From Cordilleras to Cratons</a>”, guest edited by Federico Davila, Mauricio Parra</span></strong></p><div><strong><br></strong></div><div id="ydp6bbeedaenhancr_card_4930473850" class="ydp6bbeedayahoo-link-enhancr-card ydp6bbeedayahoo-link-enhancr-not-allow-cover ydp6bbeedaymail-preserve-class ydp6bbeedaymail-preserve-style" style="max-width:400px;font-family:YahooSans, "Helvetica Neue", "Segoe UI", Helvetica, Arial, sans-serif" data-url="https://nam11.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.sciencedirect.com%2Fjournal%2Fjournal-of-south-american-earth-sciences%2Fspecial-issue%2F10CV3PKFJGV&data=04%7C01%7Cl.brett%40elsevier.com%7Caf812a6088ea4c5fa0c508d9828f3d37%7C9274ee3f94254109a27f9fb15c10675d%7C0%7C0%7C637684373998133731%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C1000&sdata=O4aNpzmu3Tn9ujOPoHuL%2FqXtZzU9mmJPbc0NwRoz6YY%3D&reserved=0" data-type="YENHANCER" data-size="MEDIUM" contenteditable="false"><strong><a href="https://nam11.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.sciencedirect.com%2Fjournal%2Fjournal-of-south-american-earth-sciences%2Fspecial-issue%2F10CV3PKFJGV&data=04%7C01%7Cl.brett%40elsevier.com%7Caf812a6088ea4c5fa0c508d9828f3d37%7C9274ee3f94254109a27f9fb15c10675d%7C0%7C0%7C637684373998133731%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C1000&sdata=O4aNpzmu3Tn9ujOPoHuL%2FqXtZzU9mmJPbc0NwRoz6YY%3D&reserved=0" style="text-decoration-line: none !important; text-decoration-style: solid !important; text-decoration-color: currentcolor !important; color: rgb(0, 0, 0) !important;" class="ydp6bbeedayahoo-enhancr-cardlink" rel="nofollow" target="_blank"><table class="ydp6bbeedacard-wrapper ydp6bbeedayahoo-ignore-table" style="max-width:400px" cellspacing="0" cellpadding="0" border="0"><tbody><tr><td width="400"><table class="ydp6bbeedacard ydp6bbeedayahoo-ignore-table" style="max-width:400px;border-width:1px;border-style:solid;border-color:rgb(224, 228, 233);border-radius:2px" width="100%" cellspacing="0" cellpadding="0" border="0"><tbody><tr><td><table class="ydp6bbeedacard-info ydp6bbeedayahoo-ignore-table" style="background-color: rgb(255, 255, 255); background-repeat: repeat; background-attachment: scroll; background-image: none; background-size: auto; position: relative; z-index: 2; width: 100%; max-width: 400px; border-radius: 0px 0px 2px 2px; border-top: 1px solid rgb(224, 228, 233);" cellspacing="0" cellpadding="0" border="0"><tbody><tr><td style="background-color:#ffffff;padding:16px 0 16px 12px;vertical-align:top;border-radius:0 0 0 2px"></td><td style="vertical-align:middle;padding:12px 24px 16px 12px;width:99%;font-family:YahooSans, "Helvetica Neue", "Segoe UI", Helvetica, Arial, sans-serif;border-radius:0 0 2px 0"><h2 class="ydp6bbeedacard-title" style="font-size: 14px; line-height: 19px; margin: 0px 0px 6px; font-family: YahooSans, "Helvetica Neue", "Segoe UI", Helvetica, Arial, sans-serif; color: rgb(38, 40, 42); max-width: 314px;">Journal of South American Earth Sciences | Thermochronology in South Ame...</h2><p class="ydp6bbeedacard-description" style="font-size: 12px; line-height: 16px; margin: 0px; color: rgb(151, 155, 167);">Thermochronology and geochronology share many theoretical and technical fundamentals (e.g., Reiners et al., 2005...</p></td></tr></tbody></table></td></tr></tbody></table></td></tr></tbody></table></a></strong></div><div><strong><br></strong></div><div><strong><br></strong></div><p></p> 
<p style="margin-right:0in;margin-bottom:9.0pt;margin-left:0in;">
Low-temperature thermochronology is an excellent proxy to understand the
 thermal evolution of the upper crust (<10 km), particularly when 
geological observations, different methods and low-temperature closure 
minerals (fission tracks and U-Th / He in apatites
 and zircons) are combined. In South America, this type of information 
has contributed to understanding mountain building and modes of 
deformation along the Andes and proto-Andes as well as the exhumations 
associated with passive and cratonic belts along the
 Atlantic margin. This special issue addresses new data, analytical and 
numerical modeling as well as novel applications in various mineral 
systems and regions of South America to attack different geodynamic and 
geological problems.</p> 
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