It suggests that the IBR is more susceptible to deeper earthquakes, while crustal-scale earthquakes are more likely to occur in the TTSZ,' the study said. In contrast, the seismicity in the Indo-Burma Ranges (IBR) is observed up to a depth of around 200 km, suggesting the active subduction (a term borrowed from oceanography, which means the tectonic process at convergent margins by which slabs of oceanic lithosphere descend into the mantle) process of the Indian plate beneath the IBR. 'The TTSZ is seismically active up to around 40 km depth. (All places in the Lohit district of Arunachal Pradesh). Another major finding was that the Mishmi, Tidding, and Lohit thrusts are steeply dipping thrust faults while the Walong fault is a strike-slip fault with a minor thrust component. The study published in Tectonophysics Journal also found that the Tidding-Tuting Suture Zone is seismically active up to approximately 40 km depth. The researchers analysed the earthquake data recorded by the local broadband seismograph network as well as reviewed catalog data of the International Seismological Center for the seismicity in the north-eastern fringe of the Indian Plate in the EHS (Tidding-Tuting Suture) and adjoining areas. The northeast corner of the Indian Plate in the EHS belongs to the seismic zone V of the national zoning map of India and has a potential to trigger major earthquakes in the future. The Eastern Himalayan Syntaxis (EHS) on the foothills of eastern Arunachal Pradesh and bordering regions of Assam is acknowledged as one of the most seismically active regions in the world. The study has also suggested that the Indo-Burma Range (IBR) is more susceptible to deeper earthquakes, while crustal-scale earthquakes are more likely to occur in the Eastern Himalayan Syntaxis (EHS). So we do that.New Delhi, Jun 2 (IANS): The subduction of the Indian Plate discontinues north of 27 N latitude and the indentation process is responsible for seismicity in region connected with the Assam earthquake of 1950 (magnitude 8.6), a study has found. Then we took that, and we reflected it across the y axis.

So we went from minus one for two, for one. We swap positions of the coordinates and we took the X coordinate and swap the sign. So we ended up with is we started with a point we wrote to that 0.90 degrees. It was here and reflected across the Y axis, and it's going to move toe over to the left side of the negative side.

Remember, for reflection across the y axis we're gonna take, um and we're just gonna change the sign of the X coordinate. And now the next step is reflected across the Y axis. Where is it gonna end up? It starts ad minus one. And so that's just Ah, it's pretty easy if we think about taking this point and rotating it 90 degrees. And when we rotate this about that origin 90 degrees where we end up with is a new point k and minus h. Okay, so remember, uh, uh, rotated point around the origin 90 degrees. So 1st 1 rotate 90 degrees, and then we want to reflect over the Y axis. And we're being asked to rotate that 90 degrees about the origin and then reflected across the y axes. And label that point minus one comma four. Hello There were given a point in this problem of minus one for good.

270 clockwise rotation