W e l c o m e t o t h e w e b p a g e o f p r o f e s s o r M i c h a e l
E-mail: mh.geoconsultoria@gmail.com
The traditional correlation is based on lithostratigraphy .
Essentially, this "classic" technique consists of joining similar types of rocks in the same unit. That's what the figure shows ...
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The sands of the two wells are seemly in contact - so why did one well is
dry and the other not?
In fact, this kind of situation happens quite often... "inexplicably" - one well is productive, and the adjacent one is not. Usually, the "solution" is to put a fault in the middle to explain the situation... But the correct thing is to make an appropriate correlation. This is possible with the proper stratigraphic tools. Below we show the same geological situation, but correlating under this different stratigraphic perspective. I can help you do that with your data!
