If the chlorine concentration is increasing and no particular cation is increasing accordingly, I would say the chance is near 100%. There have to be different chlorides contributing the chlorine to produce this distribution, I see no alternative. Cations commonly observed at Eagle Crater included sodium, magnesium, potassium, calcium, manganese, and iron. Corresponding chlorides on earth might include halite (sodium chloride), silvite (potassium chloride), rinneite (potassium sodium iron chloride), scacchite (manganese chloride), and carnallite (hydrated calcium magnesium chloride). This by no means exhausts the possibilities.