The terms troostite and sorbite are obsolete . We have at this point pearlite, upper bainite, lower bainite and martensite. In the late '60s electron microscopes became available giving us 100,000x magnification rather than the optical microscope's 1,000x .That gave us a much better idea of structures. Today we have as high a 1,000,000x .It's amasing what we can see today !!