View source for 2021 CSDMS meeting-078

{{CSDMS meeting personal information template-2021
|CSDMS meeting first name=Phaedra
|CSDMS meeting last name=Upton
|CSDMS meeting institute=GNS Science
|CSDMS meeting city=Lower Hutt
|CSDMS meeting country=New Zealand
|CSDMS meeting email address=p.upton@gns.cri.nz
}}
{{CSDMS meeting select clinics1 2021
|CSDMS_meeting_select_clinics1_2021=3) An Introduction to using Google Earth Engine
}}
{{CSDMS meeting select clinics2 2021
|CSDMS_meeting_select_clinics2_2021=2) Inclusive Mentoring
}}
{{CSDMS meeting select clinics3 2021
|CSDMS_meeting_select_clinics3_2021=1) Landscape Evolution Modeling with TerrainBento and Landlab
}}
{{CSDMS meeting abstract yes no 2021
|CSDMS meeting abstract submit=Yes
}}
{{CSDMS meeting abstract title temp2021
|Working_group_member_WG_FRG=Terrestrial Working Group, Geodynamics Focus Research Group
}}
{{CSDMS meeting authors template
|CSDMS meeting coauthor first name abstract=James
|CSDMS meeting coauthor last name abstract=Crampton
|CSDMS meeting coauthor country=New Zealand
}}
{{CSDMS meeting authors template
|CSDMS meeting coauthor first name abstract=Andy
|CSDMS meeting coauthor last name abstract=Tulloch
|CSDMS meeting coauthor country=New Zealand
}}
{{CSDMS meeting authors template
|CSDMS meeting coauthor first name abstract=Matthew
|CSDMS meeting coauthor last name abstract=Sagar
|CSDMS meeting coauthor country=New Zealand
}}
{{CSDMS meeting authors template
|CSDMS meeting coauthor first name abstract=Alison
|CSDMS meeting coauthor last name abstract=Duvall
|CSDMS meeting coauthor town-city=Seattle
|CSDMS meeting coauthor country=United States
|State=Washington
}}
{{CSDMS meeting abstract template 2021
|CSDMS meeting abstract=The Marlborough Fault System (MFS) consists of four main dextral strike-slip faults which link subduction with oblique continental collision in central New Zealand. It is a zone where crustal transfer from one plate to another is occuring, where a subduction interface is developing within a previously intact plate and which varies along and across strike. We use a variety of tools including topographic fabric, river evolution, thermochronology and geological history to understand the deformation that is occurring across the MFS. We show that the eastern and western ends of these faults have had completely different evolutions through time. These apparently continuous strike-slip faults have coalised into through going structures quite recently. The signature of these processes can be found in the landscape.
}}
{{blank line template}}