Yes, there are several case studies of tectonic settings and their geological consequences. Here are a few examples:

1. Subduction Zones:
- The Pacific Ring of Fire is a well-known tectonic setting with numerous subduction zones. These zones are known for their intense volcanic activity and large earthquakes. For example, the subduction zone off the coast of Chile has experienced several devastating earthquakes, including the 2010 earthquake with a magnitude of 8.8. The subduction of the Nazca Plate under the South American Plate in this region has resulted in the formation of the Andes Mountains and the volcanic activity in the area.

2. Divergent Boundaries:
- The Mid-Atlantic Ridge is an example of a divergent boundary, where the Eurasian Plate and the North American Plate are moving apart. This tectonic setting has resulted in the formation of a vast underwater mountain range. The separation of the plates leads to the upwelling of magma, creating new oceanic crust. Iceland is a prominent example of a landmass formed due to the volcanic activity associated with the Mid-Atlantic Ridge.

3. Transform Boundaries:
- The San Andreas Fault in California, USA, is a well-known example of a transform boundary. The Pacific Plate and the North American Plate are sliding past each other horizontally, resulting in frequent earthquakes. The 1906 San Francisco earthquake, with a magnitude of 7.8, was one of the most devastating earthquakes in history. The movement along this fault has caused significant geological consequences, such as the formation of the California Coast Ranges.

4. Collision Zones:
- The Himalayas is an example of a collision zone where the Indian Plate is colliding with the Eurasian Plate. This tectonic setting has resulted in the formation of the highest mountain range in the world. The collision has caused intense folding and faulting, leading to the formation of deep valleys, high peaks, and the development of major river systems such as the Ganges and the Indus.

5. Hotspots:
- The Hawaiian Islands are a result of volcanic activity associated with a hotspot. A hotspot is a plume of hot material rising from deep within the Earth's mantle. As the Pacific Plate moves over the hotspot, a chain of volcanic islands is formed. The Hawaiian Islands provide a classic example of how a hotspot can create a sequence of islands that become progressively older towards one end.

These case studies highlight the diverse geological consequences of different tectonic settings. From volcanic activity and earthquakes to the formation of mountain ranges and islands, tectonic processes play a significant role in shaping the Earth's surface.