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The most useful feature that covers both (a carbonate unit in India) and Torro (assuming you mean Torrowangee in Australia or a reservoir modeling context) would be Lithofacies Classification for Carbonate Sequence Stratigraphy .

# 4. Classify systems tract if stacking_trend == "upward_deepening": return "TST (good source potential if organic-rich laminites present)" elif stacking_trend == "upward_shallowing": return "HST (reservoir potential: dolomitized grainstone, common in Torro)" elif evaporite_dominant: return "LST (seal facies: anhydrite, similar to Bilara 'A' unit)" | Depth (m) | Lithofacies | System Tract | Reservoir Quality | |-----------|----------------|--------------|-------------------| | 1200-1215 | Laminated dolomudstone | TST | Poor | | 1215-1230 | Stromatolite boundstone | Early HST | Moderate (vuggy) | | 1230-1245 | Anhydrite + dolomite | Late HST | Tight (seal) | Alternative interpretation (if not geology): If you meant Bilara and Torro as software tools or frameworks (e.g., Bilara for data pipelines, Torro for testing), please clarify. The most useful feature then would be an API compatibility layer between their data models.

Based on your request, it sounds like you are referring to (a limestone formation/zone in the Jurassic period) and Torro (likely a misspelling of Torrowangee or Toroweap ? Or perhaps a specific software/library?).

Let me know your specific domain (geoscience, programming, or otherwise), and I'll refine the answer further.

# 3. Identify high-frequency shallowing-upward parasequences # (common in both Bilara and Torro dolomites) stacking = detect_fischer_plot_cycles(gr_log, cycle_height=2) # meters

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Torro: Bilara And

The most useful feature that covers both (a carbonate unit in India) and Torro (assuming you mean Torrowangee in Australia or a reservoir modeling context) would be Lithofacies Classification for Carbonate Sequence Stratigraphy .

# 4. Classify systems tract if stacking_trend == "upward_deepening": return "TST (good source potential if organic-rich laminites present)" elif stacking_trend == "upward_shallowing": return "HST (reservoir potential: dolomitized grainstone, common in Torro)" elif evaporite_dominant: return "LST (seal facies: anhydrite, similar to Bilara 'A' unit)" | Depth (m) | Lithofacies | System Tract | Reservoir Quality | |-----------|----------------|--------------|-------------------| | 1200-1215 | Laminated dolomudstone | TST | Poor | | 1215-1230 | Stromatolite boundstone | Early HST | Moderate (vuggy) | | 1230-1245 | Anhydrite + dolomite | Late HST | Tight (seal) | Alternative interpretation (if not geology): If you meant Bilara and Torro as software tools or frameworks (e.g., Bilara for data pipelines, Torro for testing), please clarify. The most useful feature then would be an API compatibility layer between their data models.

Based on your request, it sounds like you are referring to (a limestone formation/zone in the Jurassic period) and Torro (likely a misspelling of Torrowangee or Toroweap ? Or perhaps a specific software/library?).

Let me know your specific domain (geoscience, programming, or otherwise), and I'll refine the answer further.

# 3. Identify high-frequency shallowing-upward parasequences # (common in both Bilara and Torro dolomites) stacking = detect_fischer_plot_cycles(gr_log, cycle_height=2) # meters

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