Processes during shallow burial.
A True form fossil is a fossil of the whole/entire body of the organism.
This is called a trace fossil. or a mold.
Fossil
A tropites fossil is a fossil of a tropites. A tropites is a genus of coiled ammonite. They only existed for about 20 million years, which makes it a good index fossil.
deep fossil
No, while peat can be used a fuel, it is in the same class a wood it is not a fossil fuel. The form of coal that has undergone the least diagenesis (and is still a fossil fuel) is called "Lignite".
diagenesis
The cast of Diagenesis - 2011 includes: Perry Powell as Colin Kenneth Taite as Rock
organic materials
changes in sediment or a rock during and after lithificatioin
Mark Vernon Mauritsen has written: 'Studies of diagenesis of bermuda limestones' -- subject(s): Carbonate Rocks, Diagenesis, Limestone, Rocks, Carbonate
Janet K. Pitman has written: 'Diagenesis and reservoir quality of the Upper Mississippian Aux Vases Sandstone, Illinois Basin' -- subject(s): Diagenesis, Geology, Geology, Stratigraphic, Petroleum, Stratigraphic Geology 'Regional diagenetic patterns in the St. Peter Sandstone' -- subject(s): Diagenesis, Geology, Stratigraphic, Stratigraphic Geology 'Diagenesis and reservoir quality of the upper Mississippian Aux Vases Sandstone, Illinois Basin (U.S. Geological Survey professional paper)'
C.H Moore has written: 'Carbonate reservoirs : porosity evolution and diagenesis in a sequence stratigraphic framework / Clyde H. Moore' -- subject(s): Carbonate Rocks, Diagenesis, Rocks, Carbonate
George V. Wood has written: 'Diagenesis and stratigraphy of the Lisburne Group limestones of the Sadlerochit Mountains and adjacent areas, northeastern Alaska' -- subject(s): Diagenesis, Geology, Limestone, Stratigraphic Geology
Mostly the sedimentary part which involves the process of weathering, and diagenesis occurs at the earths surface.
Orogenesis: The process of mountain formation, especially by a folding and faulting of the earth's crust Diagenesis: The physical and chemical changes occurring during the conversion of sediment to sedimentary rock. So, from one geologist to a non-geologist - I'd say no.
the reason is because rocks can have different depositional environments and diagenesis history.