The first thing you need to understand is that all physically realizeable waters are electrically balanced. Thus you cannot make an unbalanced water by adding salts to any real water you have. The second most important concept is that the distribution of electrical charge in any water that contains carbo in any form i.e. carbonic, bicarbonate or carbonate or any phosphate or any sulfate though carbo is well and away the most important player depends on pH. When the profiles for Brun water were put together it is clear that the author listed the calcium, magnesium, sodium, sulfate and chloride he wanted, added up their charges and found a large net positive number. Knowing that most natural waters contain bicarbonate he balanced this positive charge with bicarbonate intending that the brewer would add sodium bicarbonate to synthesize the profile. But the profile only balances at pH 8.3 (the pH at which most of the carbo in a solution is bicarbonate). If one adds bicarbonate to water the pH shifts depending on what is already in it and goes to 8.3 only if the water is initially ion free.
But turning to your numbers: I assume they mean 50 mg/L Ca++, 5 mg/L Mg++, 10 mg/L Na+ and 200 mg/L SO4-- and 100 mg/L Cl-. The question normally at this point would be "OK; here's the stuff he wants. Now what pH does he want it at and how much carbo is it going to take to balance at that pH?". In this case, you have sulfate and chloride to the extent of -7.81 mEq/L and only +2.91 mEq/L Ca++, Mg++ and Na+ to balance them. Those levels of anion require a lot more metal to balance them and you will never get to a realizable profile unless you are more realistic about the metal amounts. If you want sulfate at 200 and chloride at 100 and want to limit Mg++ to 5 mg/L you will have to accept Ca++ at 131.6 mg/L. You can't have anything you want. Cations and anions must be in balance and are also limited by the relative amounts found in the salts we use.