Topographic and kinematic data from the Kaikoura earthquake, New Zealand (NERC grant NE/P021425/1)

In this submission we Include three data sets collected as part of a NERC Urgency programme. Data were collected from a key field site within the Marlborough Fault Zone (MFZ), New Zealand. The Mw 7.8 Kaikoura Earthquake of 14th November 2016 was characterised by a surprising degree of spatial complexity in the surface displacement field in the Marlborough region, South Island, New Zealand. This complexity includes movement on up to 12 faults, besides a high degree of variability in apparent slip along strike of individual faults over relatively short distances. The Urgency programme included rapid collection of Terrestrial Laser Scanning (TLS), Structure from Motion (SfM) and Global Navigation Satellite System (GNSS) data immediately after this event. We include data for one of our field sites for which data collection succeeded, and processing has been completed. For a summary of the key initial findings from this data set, see the following EGU 2018 Abstract and summary: https://meetingorganizer.copernicus.org/EGU2018/EGU2018-6847.pdf

在本提交中，我们包括作为NERC紧急项目一部分所收集的三个数据集。数据采集自新西兰马尔堡断层带（MFZ）的关键野外研究站点。2016年11月14日发生的Mw 7.8级凯库拉地震，以其在新西兰南岛马尔堡地区地表位移场中展现出的令人惊讶的空间复杂性而著称。这种复杂性涉及多达12个断层的运动，同时在相对较短的距离内，单个断层沿走向的表观滑移度也表现出极高的变异性。紧急项目包括在此事件发生后迅速采集地面激光扫描（TLS）、运动结构（SfM）和全球导航卫星系统（GNSS）数据。我们包括了其中一个野外研究站点的数据，该站点的数据采集成功，且处理工作已圆满完成。关于该数据集的关键初步发现，请参阅以下EGU 2018会议摘要及总结：https://meetingorganizer.copernicus.org/EGU2018/EGU2018-6847.pdf