Your cart is empty
Add prompt packs to continue
Copy, paste and use them in your favorite AI:
Just $0.08 per prompt · one-time payment
100 resources included
This collection of prompts is designed to transform the productivity of the modern geologist, eliminating technical bottlenecks in report writing, quantitative analysis, and complex data management. By focusing on the most demanding office tasks, these prompts allow you to automate the synthesis of petrographic, structural and geochemical data with superior technical precision, guaranteeing professional standards in each document generated. From the preparation of water balances to the validation of quality control (QA/QC) protocols, each prompt acts as an expert assistant specialized in critical niches of applied geology. This tool not only reduces administrative work hours, but also increases the analytical quality of the reports, allowing the professional to concentrate on high-level interpretation and strategic decision making in mining, civil and exploration projects.
Acts as an expert geologist in basin analysis and advanced sedimentary petrology. Your task is to carry out a comprehensive interpretation of the origin of the sediments for the geological unit [FORMATION_NAME] located in [GEOGRAPHIC_LOCATION]. This analysis should integrate data from modal petrography, trace element geochemistry, and detrital geochronology to reconstruct the tectonic and paleogeographic history of the source area, considering temporal and spatial variations within the basin. Begin by evaluating the mineralogical composition of the sandstones based on point counting using the [COUNTING_METHOD] method. It uses Dickinson's ternary diagrams (QFL and QmFLt) to classify the original tectonic environment, discriminating between continental blocks, magmatic arcs and recycled orogens. It is imperative that you analyze the relationship between mineral stability and the postulated [PALEOCLIMATIC_CONTEXT], discussing how chemical weathering or vigorous relief may have skewed the population of lithic fragments and feldspars in the sample. Subsequently, it integrates the whole rock geochemical data. It uses immobile element ratios such as Th/Sc, La/Th and Sc/Cr to identify the mafic or felsic affinity of the source area. Apply discrimination diagrams from [AUTHOR_GEOCHEMISTRY_DIAGRAM] (e.g., Roser & Korsch) to validate petrographic interpretations. You should pay special attention to Europium anomalies (Eu/Eu*) and light rare earth enrichment (LREE) to infer cortical differentiation processes in the source block, as well as the chemical alteration index (CIA) to quantify the intensity of weathering. Finally, it synthesizes U-Pb geochronology data in detrital zircons. Analyze age spectra and probability density curves to correlate age peaks with known orogenic events in the [CRATON_OR_ADJACENT_BELT]. Discusses the possibility of recycling older sedimentary units versus the direct contribution of crystalline basement. It concludes with a detailed paleogeographic evolution model that explains the configuration of the drainage systems and the architecture of the basin during the [GEOLOGICAL_AGE] interval. If any key information needed to fill the bracketed fields is missing, ask me the necessary questions before answering.
Instant access after purchase from your dashboard. Just copy and paste into your AI.
ChatGPT, Claude, Gemini, DeepSeek, Grok, Qwen and any AI chat.
Yes. Every prompt includes bracketed fields where you insert your own information, context and specifics, so they fit your situation, country or industry.
Yes. Above you can read full sample prompts, exactly as you'll receive them, to check the quality before paying.
Yes. Pay once and they're yours forever, updates included.
He acts as a Senior Structural Geologist with specialization in Geotechnics and Natural Resources Exploration. Your objective is to process, analyze and interpret a set of spatial orientation data measured in the field or extracted from well logs, specifically focusing on the **Strike and Dip Projection** technique within the framework of a [Project Type: e.g. Mining Slope Stability / Hydrothermal Vein Exploration / Tunnels] project. To start the analysis, you must take the following data set: [Insert Data List: Heading/Dip or Dip/Dip Direction] and perform a systematic conversion to polar coordinates if necessary. Use the [Falsilla Type: Wulff or Schmidt] falsilla to project the poles of the planes. It is essential that you identify the main families of discontinuities (sets) through pole density analysis using the [Contour Method: e.g., Kamb or Schmidt] method, accurately determining the average planes for each family detected in the [Location or Measurement Station] sector. Once the structures are designed, perform a detailed kinematic analysis to evaluate stability or structural control. If the objective is geotechnical, evaluate the susceptibility to failures of type [Fault Type: Planar / Wedge / Overturning] considering a slope with orientation [Slope Orientation] and a friction angle of [Internal Friction Angel of the material]. If the objective is exploration, determine the direction of the main stresses (Sigma 1, 2 and 3) from the geometry of the planes and the kinematics of the fault striations if they were present in the record of [Name of the Geological Unit]. Finally, it integrates these results into a regional tectonic context. Explain how the projection of these strikes and dips correlates with [Name of Tectonic Event] deformation events and what implications it has for the structural permeability model or engineering design safety factor in the [Name of Study Area] area. The final report must include the coordinates of the centers of the pole clusters and a technical description of the anisotropy of the rock mass based exclusively on the projected data. If any key information needed to fill the bracketed fields is missing, ask me the necessary questions before answering.
He acts as a Geologist Specialist in Petrography and Igneous Petrology with 20 years of experience in writing high-precision technical reports. Your objective is to generate a detailed, technical and professional description of an intrusive lithological contact between [Name of Intrusive Unit] and [Name of Host Rock]. The description must be suitable for inclusion in regional geological mapping reports or detailed petrographic studies, maintaining strict scientific rigor and using advanced geological terminology. It begins with the macroscopic description (of a hand sample or outcrop), detailing the geometric nature of the contact (net, gradational, irregular or sinuous). It analyzes the presence of cooling edges (chilled margins), specifying the reduction in the granulometry of the crystals towards the contact. It documents the existence of box rock xenoliths trapped at the margin of the intrusion, describing their size, roundness, and the degree of magmatic assimilation. It mentions whether there are apophyses or minor dykes that detach from the main body towards the host rock, as well as evidence of magmatic brecciation in the contact zone. In the microscopy section (thin section), it accurately describes the textural variations observed under the petrographic microscope (Plane and Polarized Transmitted Light). Focus on the transition of textures [Ex: Phaneritic to Aphanitic] and describe any preferential crystal orientation (flow or trachytic texture) parallel to the contact plane. It details the microscopic shear relationships and the presence of diagnostic mineral phases resulting from contact metamorphism in the case rock, such as the formation of [Contact Minerals, e.g.: garnet, cordierite, wollastonite]. Identify reaction fringes or alteration crowns on the edges of primary phenocrysts that indicate chemical imbalance. It concludes with a technical interpretation of the emplacement sequence and inferred thermodynamic conditions. Discuss the relative cooling rate and whether the contact suggests shallow (epizonal), intermediate (mesozonal), or deep (catazonal) emplacement. It integrates observations on the hydrothermal alteration associated with contact, mentioning the replacement of primary minerals by secondary phases such as [Alteration Minerals, e.g. sericite, chlorite, epidote]. The writing style should be descriptive-analytical, avoiding ambiguities and ensuring that each technical term (such as idiomorphism, intersertal or metasomatism) is correctly applied to the geological context described for the sample [Sample ID/Code]. If any key information needed to fill the bracketed fields is missing, ask me the necessary questions before answering.
It's a master instruction, optimized for AI.
Prompt
your instruction
AI
Result
Based on 6 reviews
It's fine, nothing more. I had to tweak them quite a bit for my case. Works if you customize it.
It does the job, though I expected a bit more. They work as a starting point. Could be better but useful.
It's fine, nothing more. Some prompts are great and others more generic. Could be better but useful.
I didn't expect them to be this complete. They're easy to adapt to my case by just changing the fields. One hundred percent recommended.
Exceeded my expectations. They work just as well in ChatGPT and Claude. An investment that pays for itself.
Good value for money. The prompts are useful and practical. I'd buy again.