1988 Tennant Creek earthquakes

Sequence of strong quakes in Northern Territory October 2022 -19.81 133.89 region:Australia inline, title Northern Territory#Australia 22 January 1988 45 seconds (mainshock)http://www.emknowledge.gov.au/resource/?id=465 Resource – Australian Emergency Management Knowledge Hub 10 June 2013 5 March 2016 https://web.archive.org/web/20160305225146/https://www.emknowledge.gov.au/resource/?id=465 dead 10:06 13:57 22:05 Lake Surprise and Kunayungku faults Thrust Northern Territory, Australia $1 millionBowman J. R. 14 November 1991 The 1988 Tennant Creek, northern territory, earthquakes: A synthesis https://www.tandfonline.com/doi/abs/10.1080/08120099208728056 Australian Journal of Earth Sciences 39 5 651–669 10.1080/08120099208728056 26 August 2022 subscription 9Significant Earthquake Information https://www.ngdc.noaa.gov/hazel/view/hazards/earthquake/event-more-info/5157 National Centers for Environmental Information 26 August 2022 More than 15,000, the biggest being b yes 5.8 200px Surface rupture caused by the earthquakes 1988-01-22 00:36:00 1988-01-22 03:57:28 1988-01-22 12:05:00 usp0003c94 usp0003c9b usp0003c9n 6.2 w yesISC-GEM Global Instrumental Earthquake Catalogue (1900–2012) http://www.isc.ac.uk/iscgem/index.php ISC 2016 International Seismological Centre Version 3.0 6.3 w yes 6.6 w yes 448554 448569 448602 None On 22 January 1988, a sequence of destructive earthquakes measuring 6.2, 6.3, and 6.6 struck southwest of Tennant Creek, Australia which was felt as far north as Darwin and in other regions of the country. The largest event of the sequence was the largest earthquake ever recorded in mainland Australia since records began in 1800. Tennant Creek 1988 earthquake now Australia's biggest after Geoscience revises list ABC News Australia 12 May 2016 https://www.abc.net.au/news/2016-05-12/northern-territory-1988-quake-now-rated-australias-biggest/7406988 26 August 2022 An intensity of IX (Violent) was observed. Despite the large magnitude of the earthquakes and a close proximity to a town, in a country where earthquakes of this size are not common, damages were limited. Thousands of aftershocks were reported across the Northern Territory. Tectonic setting Geology of Australia The continent of Australia borders some very seismically active regions, such as the boundary between the Pacific and the Australian plate where both plates collide, which runs from the island of New Guinea all the way to New Zealand. On the south and west sides of it are moderately active mid-ocean ridges which run through the Indian Ocean. However, the continent does not border these and is intraplate therefore occurrences of large earthquakes are rather rare. Despite the low seismicity, most large earthquakes which occur within Australia are scientifically significant. A few earthquakes of magnitude 5 occur yearly on average, and smaller, local earthquakes can occur daily and be detected by seismograms. Doyle H. A. Everingham I. B. Sutton D. J. 30 July 1968 Seismicity of the Australian continent https://www.tandfonline.com/doi/abs/10.1080/00167616808728700 Journal of the Geological Society of Australia 15 2 20 10.1080/00167616808728700 1968AuJES..15..295D 26 August 2022 subscription These big earthquakes near Tennant Creek occurred in the Proterozoic North Australian Craton, approximately 1500 km further south than the nearest plate boundary, therefore these events are referred to as intraplate earthquakes. The area where the quakes struck had no history of any earthquake before 1986 compared to the other seismic zones that have had bigger quakes which were seismically active beforehand. Bowman J. R. 14 November 1991 The 1988 Tennant Creek, northern territory earthquakes: A synthesis https://www.tandfonline.com/doi/abs/10.1080/08120099208728056 Australian Journal of Earth Sciences 39 5 651–669 10.1080/08120099208728056 26 August 2022 subscription The Tennant Creek fault zone which includes the Kunayungku and Lake Surprise faults which were ruptured, is located on the border between a Palaeozoic basin and an early Proterozoic Tennant Creek inlier which is surrounded by younger rocks. Both of these areas are a part of the North Australian Craton, which has formed a single stationary block of crust for 1,700 million years. The inlier is a basement of another bigger feature and consists of a group made up of sedimentary and metasedimentary rocks which is the Warramunga group which is intruded by older granite. Cambrian sedimentary platform sequences of the Palaeozoic Wiso Basin overlaps the Tennant Creek inlier on the western side near the fault scarps located in the region forming an extensive transition zone. The focal depths of the Tennant Creek sequence ranged from 3.5 to 6.5 km, which is deeper than the thickness of the Cambrian platform near the epicenter. This proves that rather than the basin sedimentary, the Proterozoic basement controlled the nucleation of rupture. Earthquakes The sequence created two scarps on the faults; the Lake Surprise scarp on the southern side in a boomerang shape looked from bird's eye and the Kunayungku scarp on the northern side which is shorter than Lake Surprise. On the west-northwest trending scarps, the Lake Surprise scarp was lifted as much as 2 meters compared to the northern one and a trench across the southern LS (Lake Surprise) scarp revealed a thrust plane that was dipping 20 to 30 degrees. No scarp was found when the pipelines that got damage were being surveyed. Other articles describe the aftershock zones as dipping towards the southwest at 40 to 50 degrees from the west-northwest trending ruptures. The east-northeast trending Western LS scarp did display a left lateral strike-slip motion but dip-slip was the dominant characteristic. The slip on the Western LS fault from observations in the area was thought to be facing northward, opposite to that observed on the scarps trending west-northwest. It is interpreted that the preliminary epicenters of the aftershocks are displaying a northwest dip for the Western LS fault which concludes that it is a thrust fault which also proves, along with focal mechanisms inferred from waveform data, that the focal mechanism of the 3 main shocks are thrust, oblique thrust and thrust in order. McCaffrey R. May 1989 Teleseismic investigation of the January 22, 1988 Tennant Creek, Australia, earthquakes https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/GL016i005p00413 Geophysical Research Letters 16 5 413–416 10.1029/gl016i005p00413 1989GeoRL..16..413M 26 August 2022 subscription Aftershocks In the following year after the sequence, more than 15,000 aftershocks were recorded by the nearby Warramunga seismic array, with some aftershocks exceeding the magnitude 5 mark. The aftershocks include a 5.8 which occurred 8 hours after the biggest and last mainshock, a 5.5 occurring a week after and a 5.2 occurring later in the year at September 30.Bowman J. R. Gibson G. Jones T. 20 July 1989 Aftershocks of the 1988 January 22 Tennant Creek, Australia intraplate earthquakes; evidence for a complex thrust-fault geometry Geophysical Journal International 100 1 10 10.1111/j.1365-246X.1990.tb04570.x free thumb|300px|left|Crimped pipeline following the sequence Impacts As a result of the events, lengthy surface ruptures measuring up to 32 km were observed along the faults. Pipelines were heavily damaged as a result of the surface ruptures. Tennant Creek's hospital was seriously damaged. A few other homes were lightly damaged. No injuries or deaths were reported and US$1 million of damage was caused. Gallery Images from the Gavin Carpenter Collection on Wikimedia Commons, all images taken immediately after the initial quakes: See also List of earthquakes in 1988 List of earthquakes in Australia Earthquakes in Western Australia References Further reading Anthony J. Crone Michael N. Machette J. Roger Bowman Geologic Investigations of the 1988 Tennant Creek, Australia, Earthquakes-Implications for Paleoseismicity in Stable Continental Regions https://pubs.usgs.gov/bul/2032a/report.pdf United States Geological Survey 1992 External links 448554 (First shock) 448569 (Second shock) 448602 (Third and strongest shock) Category:1988 earthquakes Category:Earthquakes in Australia Category:January 1988 in Oceania Category:1988 in Australia Category:Tennant Creek Category:1980s in the Northern Territory Category:Earthquake clusters, swarms, and sequences