Relogging of the Butler Property Outcrops - Northern Ontario

Matthieu Cedou, Dominique Fournier, Thomas Campagne, Maria Soto Arrojo

Introduction

In mineral exploration projects, historical geological descriptions often remain an underutilized source of geological information, despite containing valuable observations recorded directly in the field. Text-based records, which are often variable in detail and structure, provide firsthand geological context on lithologies, structures, mineralization, and alteration.

Using Large Language Model applications (LLM) from Geoscience ANALYST Pro Geology, structured geological information can be extracted from poorly formatted descriptions. This approach models and organizes the geological information contained within the descriptions without relying on existing interpretive reports. This enables building an independent geological synthesis directly from historical field data, supporting exploration targeting and domain modelling workflows in a systematic, scalable manner.

This case study examines historical data from the Butler Property, made available by the Geological Survey of Ontario. The project is located in the Ring of Fire region of the James Bay Lowlands, Northern Ontario. The Butler dataset includes a total of 121 outcrop logs, each sample provided with a geographic location and a geological description. As demonstrated in the Table 1, the descriptions vary greatly in quality: from (ACE geologist) detailed lithological, structural, and mineralization observations, to (LAX geologist) minimal and vague information.

Table 1 Examples of two geological descriptions of varying quality from two different geologists.

Geologist	Description	Code
ACE	Small flat outcrop. Massive, fine-grained, grey-green magnetic siltstone to sandstone. Blebby cubic pyrite occurs along fracture planes. Cross cut by pegmatitic diorite trending at 020.	S3c
LAX	sml o/c of cg anth alt’d rock (intrusive?)	V

This examplifies one of the key challenges associated with historical data compilation: the variability in the quality and detail of geological observations.

Note

This document demonstrates and assesses the capabilities of the Relog Descriptions and Summarize using LLM applications in Geoscience ANALYST Pro Geology. For the purpose of this evaluation, we use the application in single-pass mode, with no post-processing, manual corrections, or iterative refinements. We retain initial outputs exactly as generated to objectively evaluate the system’s baseline performance. This approach is intentional: our goal is to validate the applications under realistic, uncontrolled conditions. In operational settings, outputs would be subject to systematic quality control to ensure geological consistency and interpretive reliability.

Butler Property

As presented in Fig. 1 (A), the Butler Property alies within the Butler Assemblage (2,828 Ma) of the McFaulds Lake Greenstone Belt, part of the broader Ring of Fire region in Northern Ontario. It is located between the western and eastern limbs of a folded volcanic–intrusive sequence, bounded to the north by the Webequie Shear Zone and encompassing a large tonalitic core (~2,773 Ma) in its central–eastern portion (Downey et al., 2020), as shown in Fig. 1 (B).

Fig. 1 (A) Location of the Butler property in the Canada Greenstone Belt and (B) Geological map of the Butler property (Downey et al., 2020).

The property resides within a complex geodynamic (Downey et al., 2020) environment characterized by :

• Mantle plume activity (~2,735 Ma) affecting the North Caribou microcontinent margin.

• Extensive ultramafic sills and dykes (dunite, peridotite, pyroxenite, chromite) structurally above mafic–ultramafic conduit systems.

• Varied sulfide deposits—including magmatic Ni–Cu–PGE and volcanogenic Massive Sulfide (VMS) systems formed along high-T volcanic and intrusive assemblages.

• Regional deformation marked by isoclinal folds and dextral movement along the Webequie Shear Zone.

The Butler Property’s lithostratigraphy consists of:

• Basal intrusive suite: ultramafic to ferrogabbro–gabbro cumulates forming layered intrusions.

• Intermediate to felsic volcanic rocks: including tuffs, lapilli, breccias, and flows, hosting multiple VMS horizons.

• Sedimentary and siliciclastic units interlayered with volcanic strata.

• Capping ferrogabbroic sill showing igneous layering suggestive of east-dipping younging direction.

• Hydrothermal alteration assemblages: biotite±anthophyllite–cordierite–chlorite–garnet zones within exhalative horizons.

In 2018, the exploration program comprised:

• Relogging of historical drill core from Butler occurrences 1–10.

• Geological outcrop mapping and sampling, targeting tonalitic intrusives, volcanic caprocks, and alteration zones (those outcrops are the one used in the present report).

• Spatial synthesis to build a unified model of stratigraphy, intrusive architecture, alteration, and mineralization potential.

The combined core and surface data informed enhanced targeting and mineralization zoning across both Cu–Zn–Ag–Pb VMS occurrences (Butler 1–4) and Ni–Cu–PGE–Ti–V–Cr targets (Butler 5–8).

Note

The Butler report was used exclusively for validation and was not injected in any data processing, except for the Geological outcrop descriptions table used as input.

Applying LLM on Butler Property outcrops

Given the inherent complexity of the information provided in individual logs, we proceed with a three-level approach that gradually focuses the queries made to the LLM. The LLM used in the present case study is OpenAI o4-mini.

The following sections demonstrate each step in detail.

• Summarize: Get a broad description of the geological context

• Categorize: Define the main geological themes

• Relog: Reformat all logs based on pre-defined categories

Note

• These applications integrate external LLM providers, either via remote APIs or local deployments, as part of a broader processing pipeline.

• Output quality and response time depend on the LLM model used and its configuration.

• The privacy policies of external LLM providers are determined solely by those providers and are independent of this application.

Summarize

First, to have an overview of the present geology, we used the Summarize using LLM application. This application extracts information from descriptions and summarizes it. The interface is presented in Fig. 2.

Fig. 2 Interface of the ‘Summarize using LLM’ application in Geoscience ANALYST Pro Geology. The application allows users to extract information from descriptions and summarize it using a LLM.

The summary provided by the LLM is the following (computing time: 44 seconds):

The mapped corridor exposes a polyphase mafic–intermediate–felsic magmatic pile with intercalated volcanic, volcaniclastic and sedimentary horizons, all overprinted by deformation, hydrothermal alteration and late‐glacial scouring.
1. Mafic Intrusive Complexes
 - NS–NE–trending bodies of coarse‐ to megacrystic gabbro–ferrogabbro–pyroxenite ± anorthosite.
 - Compositional (feldspar-rich vs. feldspar-poor) and modal layering tops to W–SE (dips ~30–48°/80°).
 - Ferrogabbro intergrowths host disseminated to massive magnetite (locally chalcopyrite blebs); coarse layers contain pyroxene phenocrysts and clots.
 - Late, fine-grained chlorite-altered gabbro pods and narrow tonalite–dacite sills cross-cut main masses.
2. Intermediate to Felsic Intrusives
 - Medium- to coarse-grained biotite-rich granodiorite–monzodiorite–tonalite bodies: massive to weakly foliated, non-magnetic, locally enclosing mafic xenoliths.
 - Aplite–pegmatite dykes (strikes ~270/090), quartz-feldspar diorite sills (020–055), and narrow aplite/quartz veins cross-cut all units.
3. Volcanic and Volcaniclastic Assemblages
 - Fine- to medium-grained flow-banded dacite–rhyolite (bedding ~078/80), locally porphyritic and amygdaloidal, cut by aplite dykes.
 - Thick lapilli- and ash-tuff packages, well foliated/crenulated (foliation ~240°), with chlorite–sericite–magnetite alteration.
 - Andesitic pillow lavas and flow breccias bearing chlorite–epidote–anthophyllite assemblages.
4. Sedimentary and Reworked Units
 - Very fine-grained, magnetic mafic siltstone/sandstone: bedding ~290°, north-up grading
locally massive. Cross-cut by medium- to coarse-grained diorite.
 - Interbeds of quartz arenite, mafic siltstone and felsic tuffs (bedding ~220–256/80), locally tightly folded.
5. High-Grade Metamorphic and Basement Rafts
 - Blocky felsic volcanic boulders (pink-grey flows) and coarse granite–granodiorite gneiss along river margins.
 - Possible migmatitic basement with mafic block rafts within dioritic bodies.
6. Structural Fabric, Alteration and Glacial Overprint
 - Regional foliations 005–238°, strong magnetite foliation at ~038/80. Discrete chlorite–carbonate–pyrite–quartz shear zones with quartz “ladder” veins.
 - Pervasive chloritization of mafic units
biotite–chlorite in gabbros, anthophyllite–chlorite in felsic flows
sericitization in tuffs.
 - Glacial striae on mafic and felsic outcrops oriented ~170–190°

Defining a proper benchmark for validating such a summary remains inherently difficult. Ideally, a geologist attempts the same task using only the outcrop descriptions to produce a comparable synthesis. However, this raises several challenges: (1) different geologists emphasize different aspects, and (2) determining which information to retain or discard involves subjective judgment and implicit thresholds. Despite these limitations, readers may still refer to the official report for comparison. However, it is important to note that the report’s geological summary does not rely solely on outcrop descriptions. It integrates additional data sources such as literature, drill core observations, and geophysical interpretations.

To compare the results of the summary, readers can refer to the geological context provided in the original report, available in the section geological setting of the Butler property.

Categorize

To extract information from the outcrop descriptions, the first step is to define which categories to target. This step uses the Question tool in the Summarize using LLM application, as illustrated in Fig. 3. Four distinct classes are defined: Lithology, Alterations, Minerals, and Texture. For each class, the prompt submitted is: What are precisely the present [class]?

Fig. 3 Interface of the Summarize application and ‘Question’ tool in Geoscience ANALYST Pro Geology. The application allows users to ask questions to a LLM and retrieve answers.

The categories for each class retrieved by the model are presented in Table 2 (computing time for the lithology category: 1 minute and 12 seconds). The model identifies a total of 21 lithological categories, 5 alteration categories, 12 mineral categories, and 12 texture categories.

The application answers the questions in a structured way, as presented in the Table 2. The categories are organized hierarchically, with the main lithological classes (plutonic, volcanic, metasedimentary/metamorphic, and sedimentary) further subdivided into specific lithologies. Textures are also organized in a hierarchical manner.

To use this categories as input for the Relog Descriptions application, the structure of the table is removed and only the categories are kept. Moreover, some categories are manually removed before using them in the Relog Descriptions application. Those fields are in italic in the table.

Table 2 Categories of geological information extracted from the Butler property outcrop descriptions by the ‘Summarize using LLM’ application.

Lithology	Alterations	Minerals	Textures
Plutonic (intrusive) A. Mafic–Ultramafic Gabbro Melagabbro Ferrogabbro Pyroxenite Anorthosite Diorite Monzodiorite Microtonalite B. Intermediate–Felsic Tonalite Granodiorite Granite Aplite Volcanic (extrusive) A. Mafic Basalt B. Intermediate–Felsic Andesite Dacite Felsic volcanic rock Felsic/intermediate tuff Metasedimentary / Metamorphic Felsic gneiss Chlorite-schist Sedimentary Quartz sandstone/quartz arenite Siltstone	Chloritization Garnet alteration Magnetite alteration Anthophyllite alteration Magnetite Amphibole alteration of pyroxene	Amphibole Biotite Calcite Chalcopyrite Chlorite Garnet Hornblende Magnetite Plagioclase Potassium feldspar Pyrite Pyroxene Quartz	1. Grain-size Textures Phaneritic Aphanitic Porphyritic 2. Primary Fabric Textures Massive Layered / Banded Foliation / Schistosity 3. Volcanic–Pyroclastic & Related Dyke Veins Lapilli-tuff / tuff Flow breccia Pillow Sugary

Relog Descriptions

The categories identified by the LLM are retrieved using the Relog Description application. The process is conducted in two steps.

Lithologies

First, as shown in Fig. 4, three lithological classes are extracted: Main lithology, Secondary lithology, and Third lithology—corresponding respectively to the dominant lithology observed in the outcrop and any additional lithologies present due to local intrusions or subordinate occurrences. A contextual prompt clarifies the hierarchical relationship between these categories. For each category, a confidence score reflects the model’s certainty regarding the relogged class. This score helps users identify results that may require closer examination, particularly in cases where the description is ambiguous or poorly structured.

Fig. 4 Interface of the ‘Relog Description’ application in Geoscience ANALYST Pro Geology for relogging lithologies. The application allows users to extract lithological information from geological descriptions using a LLM.

Alteration, Minerals, and Textures

Second, as presented in Fig. 5, the Relog Description application extracts the remaining three categories: Alterations, Minerals, and Textures. For this step, a multi-label approach applies. Since multiple minerals or alteration types can coexist at a given location, asking the LLM to assign a single label per category is not appropriate. Instead, the model is prompted to identify all categories explicitly present in each description.

Fig. 5 Interface of the ‘Relog Description’ application in Geoscience ANALYST Pro Geology for relogging alterations, minerals, and textures. The application allows users to extract multiple geological features from descriptions using a LLM.

Results

The complete results are available in the Geoscience ANALYST workspace and in this spreadsheet. The following section presents a qualitative overview of the results obtained from the Relog Description application.

Main lithologies

For each of the 121 outcrops, a Main, Secondary, and Third lithology are assigned by the Relog Description application. A confidence score (low, medium, or high) is also assigned to each category (computing time: 41 seconds). The first rows of the results are presented in Table 3.

Table 3 First rows of the results obtained from the Relog Description application for the Butler property outcrops.

#	Description	Main Lithology	Conf.	Secondary Lithology	Conf.	Third Lithology	Conf.
1	mod sized o/c of fg dacite (locally amyg) and mcg anth-alt’d int flow	Dacite	high	Andesite	medium	Unknown	Unknown
2	Old basement lithology? Migmatite shollen or raft texture. Mafic blocks with felsics squished out in between.	Felsic gneiss	low	Unknown	low	Unknown	Unknown
3	smal o/c on W side of pond. combination of cg anth-alt’d volcanic & fg siliecous non-mag felsic tuff	Felsic volcanic rock	medium	Felsic/intermediate tuff	medium	Unknown	Unknown
4	W edge of river, large blocky bldrs of fg pink-grey felsic volcn, possible flow txts	Felsic volcanic rock	medium	Unknown	Unknown	Unknown	Unknown
5	sml o/c in river of strongly re-crystallized & slightly defomred flow-banded and in-situ bx’d dac/rhy. flow banding at 078/-80. unit cut by aplite dyke @ 040-/90. Looks like hunting camp here	Dacite	medium	Granite	medium	Unknown	Unknown
6	4x4m flat bldr of str shr’d felsic volcanic with discrete chl-cct+/-pyr shears & qz ladder vns perp to shears (could this deform & veining be related to the WB shear?). 2 assays samples taken for gold (#130253, #130254)	Felsic volcanic rock	high	Unknown	low	Unknown	Unknown
7	huge o/c ridge on SE side of lake consisting of mg massive, w-str mag ferrogabbro & gabbro, crude layering defined by variation in mt distribution	Ferrogabbro	medium	Gabbro	medium	Unknown	Unknown
8	huge flat o/c of mcg massive to weakly layered melagabbro with minor thin zones of massive mt and wider zones of dissem mt. NE o/c exposes ct with microdiorite/dacite. W o/c exposes ct with microdiorite/dacite @ 190/-90. Late aplite dykes @ 270/-90 &	Melagabbro	high	Diorite	medium	Dacite	medium

The results obtained are overall fairly accurate. As expected, the confidence scores are lower for the secondary and third lithologies, reflecting the model’s uncertainty when these are detected. The only notable misclassification in the sample set remains the assignment of “Granite” as a secondary lithology instead of the “Aplite” (description 5). This remains understandable given that the primary distinction between the two lies in grain size. Finally, the confidence score associated with the main lithology also highlights cases where the original descriptions are ambiguous or lack sufficient detail.

Multi-labels

For each 121 outcrops, alteration, minerals and structures has been detected by the application (computing time: 1 minute and 20 seconds).

The Table 4 presents a sample of the results for the alteration category . Overall, most alterations remain correctly identified. The LLM misses only one instance of garnet alteration, embedded in the phrase “med sized o/c of chl-gt alt’d schist” in description 11. Additionally, magnetite (noted as “mag” in the descriptions) is not mapped as magnetite alteration. This omission remains justifiable, as the presence of magnetite is not necessarily indicative of alteration. It can be primary, particularly in magnetite-bearing lithologies such as ferrogabbro.

Table 4 Alteration found by the Relog Description algorithm; the full classes names ‘amphibole alteration of pyroxene’, ‘Chloritization’, ‘garnet alteration’, ‘magnetite alteration’, ‘anthophyllite alteration’ were shortened in the table for clarity

#	Description	Amphibole	Anthophyllite	Chloritization	Garnet	Magnetite
9	Medium to coarse grained, massive, white-grey anorthositic gabbro. Pyroxene clots protrude from the surface with plagioclase recessively weathered. Pyroxene appears partially altered to amphibole.	X
10	Medium to coarse grained, massive, white-grey anorthositic gabbro. Pyroxene clots protrude from the surface with plagioclase recessively weathered. Pyroxene appears partially altered to amphibole.	X
11	med sized o/c of chl-gt alt’d schist & mcg anth alt’d int flow(?), w-mod mag		X	X
12	v.lg smoothed o/c of v.d.green fg non-basalt, possible flow bx txt locally. glacial striae @ 170. pervasive chl altn			X
13	sml o/c W of lake, str anth alt’d volcanic (unknown protolith but likely int/felsic flow). v.wk mag. minor qz veins (10–20 cm) trending 180/-90 or 054/-65.		X
14	lg flat o/c of fmg highly siliceous weakly fol’d non-mag felsic sandstone or dacite/hypabyssal intrusive. Compositionally very uniform, no obvious bedding. Weathered surface is granular (quartz > feldspar). No significant alteration. Glacial striae @ 180.

Misclassified Lithologies

The results from the Relog Description application are compared with the lithologies originally logged by the geologist. To enable the evaluation, the lithology codes are simplified and converted to their corresponding names. When multiple lithologies are assigned as Main Lithology, only the first is considered. This allows direct alignment with the output from the Relog Description application. The comparison yields a 68.5% match between the two lithological interpretations.

The Table 5 presents examples where the lithological classifications from the geologist and the LLM differ. Upon close inspection of the original descriptions, several discrepancies suggest that the LLM’s outputs are more consistent with the textual evidence than the geologist’s assigned categories. In those cases, the LLM identifies lithologies that reflect the geological description more accurately.

Table 5 Example of differences between geologist logged geology and the log obtain with the LMM.

#	Description	Geologist Log	LLM Log
1	Medium to coarse grained, massive, white-grey anorthositic gabbro. Pyroxene clots protrude from the surface with plagioclase recessively weathered. Pyroxene appears partially altered to amphibole.	Ferrogabbro	Anorthosite
2	Medium to coarse grained, massive, white-grey anorthositic gabbro. Pyroxene clots protrude from the surface with plagioclase recessively weathered. Pyroxene appears partially altered to amphibole.	Ferrogabbro	Anorthosite
3	med sized o/c of chl-gt alt’d schist & mcg anth alt’d int flow(?), w-mod mag	Andesite	Chlorite-schist
4	v.lg smoothed o/c of v.d.green fg non-basalt, possible flow bx txt locally. glacial striae @ 170. pervasive chl altn	Basalt	Chlorite-schist
5	sml o/c W of lake, str anth alt’d volcanic (unknown protolith but likely int/felsic flow). v.wk mag. minor qz veins (10–20 cm) trending 180/-90 or 054/-65.	Unknown	Dacite
6	lg flat o/c of fmg highly siliceous weakly fol’d non-mag felsic sandstone or dacite/hypabyssal intrusive. Compositionally very uniform, no obvious bedding. Weathered surface is granular (quartz > feldspar). No significant alteration. Glacial striae @ 180.	Microtonalite	Dacite
7	Medium grained, massive, white, grey, green diorite to leucogabbro. Non-magnetic. Knobby texture.	Anorthosite	Diorite

These cases highlight potential biases or inconsistencies introduced during manual logging and suggest that the LLM, in some instances, provides a classification more consistent with the descriptive text. This raises a broader issue: the distinction between the described lithology and the assigned lithology. If the descriptions contain more precise geological observations—such as mineral proportions, textures, or contact relationships—both a geologist and the LLM can assign lithological classifications with greater confidence and accuracy.

Spatial interpretation

The Relog Description application assigns geological values to each point representing an outcrop. To visualize the spatial distribution of these values and identify potential trends, the points are interpolated onto a 2D grid using the Neural Kriging application available in Geoscience ANALYST Pro Geology.

Lithologies

Once relogged, the point data are interpolated using the Neural Kriging application, incorporating magnetic data as secondary variables, as shown in Fig. 6. Although the spatially uneven distribution of outcrops limits the accuracy of geological interpolation, this representation provides a useful overview of the regional distribution of geological units.

Fig. 6 Spatial interpolation of the main lithologies identified by the Relog Description application on the Butler property; magnetic data used as secondary data during interpolation is projected in the background.

The interpolated lithologies show, from South to North, a sequence consisting of sedimentary clastic rocks, a major granodioritic intrusion, followed by mafic intrusive rocks. The presence of intermediate to felsic volcanic rocks along the northern and western edges of the triangular zone is defined by positive magnetic anomalies.

Prospective targets

To define prospective areas, the presence of anthophyllite, chlorite, and garnet alterations, as well as veining, is interpolated using the Neural Kriging application. The Fig. 7 illustrates the results of this interpolation. These interpolations highlight two zones of interest shown in Fig. 7: (1) to the north and (2) to the west of a triangular-shaped magnetic low anomaly, bounded by linear positive magnetic anomalies at the center of the property. These alteration anomalies are spatially correlated with the felsic and intermediate volcanic rocks interpolated in the previous section. On the southeastern flank of this magnetic anomaly, chalcopyrite was observed in an outcrop (3), in association with basalt and ferrogabbro.

Fig. 7 Interpolated presences of anthophyllite, chlorite, garnet, and veining define prospecting targets; an outcrop with chalcopyrite is also projected; magnetic data is projected as background

The presence of veining, chloritization, and intermediate volcanic rocks (dacite) in the northern target (1) area may indicate a hydrothermal system consistent with an exhalative mineralization environment (Ross et al., 2019), possibly represents a distal VMS setting. In the western target (2), the combination of anthophyllite, chlorite, and garnet alteration within intermediate volcanics suggests a more proximal hydrothermal zone (Hokka, 2020), potentially closer to the feeder system. Lastly, the occurrence of chalcopyrite associated with basalts and ferrogabbro on the southeastern flank (3) may represent a distinct mineralization style, likely magmatic-hydrothermal origin (Namur et al., 2012).

Prospectivity targets validation

The Fig. 8 presents the targets identified in the 2018 report. Comparing with the targets inferred from surficial outcrop descriptions alone, a correspondence is observed with Butler 1-2 with target 1, Butler 3 with target 2, and Butler 6 with target 3. Butler 1 and Butler 3 are related to exhalative horizons, while Butler 6 is associated with remobilized or hydrothermal sulfides at the contact between ferrogabbro and tonalite intrusions (Downey et al., 2020). Those observations remain similar to the ones obtained with the LLM using outcrop descriptions only.

Following manual inspection of the outcrop descriptions, no supporting evidence emerges for the remaining targets listed in the original report, as they were targeted and identified through drill core observations and geophysical data.

Fig. 8 Targets defined during the 2018 drill core relogging and geological mapping campaign on the Butler property; previously found targets are projected on the map.

Discussion

This study demonstrates that LLMs can extract structured geological information from historical outcrop descriptions, even when the text is inconsistent or incomplete. By applying engineered LLM application, key attributes such as lithology, alteration, minerals, and texture are retrieved. The inclusion of a confidence score provides a practical measure of reliability, allowing users to identify uncertain outputs.

Once relogged, the extracted data are interpolated spatially using Neural Kriging. This approach allows the construction of a preliminary geological model directly from descriptive text. The identified targets show spatial correlation with known exploration zones (e.g., Butler 1, 3, and 6), supporting the relevance of the method in early-stage interpretation, particularly in historical datasets.

However, the LLM’s performance strongly depends on the quality of the input descriptions. Incomplete, vague, or poorly structured observations lead to inconsistent outputs; similar to the limitations faced by human interpreters. LLM outputs reaffirm a long-standing truth: the quality of geological interpretation—manual or automated—can only match the quality of the original field descriptions. When encountering an outcrop, the best investment remains a clear, detailed, and objective description.

Conclusion

Geology is a naturalistic science, grounded in the direct observation and description of rocks and their relationships. To simplify interpretation and enable digital workflows, these observations are often reduced to categorical fields, introducing a degree of interpretation. Selecting a lithology name, for instance, is a subjective decision.

Yet, while classifications may shift over time, precise, factual observations remain stable and valuable. With LLMs, geologists re-inject these observations into their workflow more effectively, transforming descriptive text into structured inputs for modelling and targeting. This unlocks the full potential of historical records—provided the descriptions are clear and rigorous.

Geologist	Description	Code
ACE	Small flat outcrop. Massive, fine-grained, grey-green magnetic siltstone to sandstone. Blebby cubic pyrite occurs along fracture planes. Cross cut by pegmatitic diorite trending at 020.	S3c
LAX	sml o/c of cg anth alt’d rock (intrusive?)	V

Ultimately, as illustrated in the table above, the success of LLMs in geology is not solely about the algorithms or models used, but rather about the quality of the geological fieldwork and observations. Accurate, objective, and detailed descriptions are essential for effective interpretation and modelling. So, as geologists, don’t be LAX, be ACE.

References

Downey M., Weston R., Heggie G., Deller M., 2020. *Butler Property 2018 Phase 2 Exploration Report: Drill Core Relogging & Geological Mapping*. Noront Resources Limited, 341 pages.

Hokka J., 2020. *Geology, alteration and lithogeochemistry of the Paleoproterozoic Korpela VMS occurrence in Eastern Finland*. Miner Deposita 55, 1581–1604.

Namur O., Charlier B., Holness M.B., 2012. *Dual origin of Fe–Ti–P gabbros by immiscibility and fractional crystallization…*. Lithos 154, 100–114.

Ross P.-S., Boulerice A., Mercier-Langevin P., McNicoll V., 2019. *Volcanology, chemo-stratigraphy, geochronology…*. Mineralium Deposita.